text:
|2006 Pacific hurricane season
Season summary map
|Seasonal boundaries
|First system formed
|May 27, 2006
|Last system dissipated
|November 20, 2006
|Strongest storm
(Most intense hurricane in the Central Pacific)
|• Maximum winds
|160 mph (260 km/h)
(1-minute sustained)
|• Lowest pressure
|915 mbar (hPa; 27.02 inHg)
|Seasonal statistics
|Total depressions
|25, 1 unofficial
|Total storms
|19, 1 unofficial
|Major hurricanes
(Cat. 3+)
|Total fatalities
|14 total
|Total damage
|$355.1 million (2006 USD)
|Related articles
The 2006 Pacific hurricane season was the most active since 2000, producing 19 tropical storms or hurricanes.[1] Eighteen developed within the National Hurricane Center (NHC) area of warning responsibility, which is east of 140°W, and one storm formed between 140°W and the International Date Line, which is under the jurisdiction of the Central Pacific Hurricane Center (CPHC). Of the 19 total storms, eleven became hurricanes, of which six attained major hurricane status. Within the NHC portion of the basin, the season officially began on May 15, and in the CPHC portion, it started on June 1; the season officially ended on November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the eastern Pacific basin.
The strongest storm of the season was Hurricane Ioke, which reached Category 5 status on the Saffir-Simpson scale in the central Pacific Ocean; Ioke passed near Johnston Atoll and later Wake Island, where it caused heavy damage but no deaths. The deadliest storm of the season was Hurricane John, which killed six people after striking the Baja California Peninsula, and the costliest storm was Hurricane Lane, which caused $203 million in damage in southwestern Mexico (2006 USD, $257 million 2020 USD).
Seasonal activity began on May 27, when Tropical Storm Aletta formed off the southwest coast of Mexico. No storms formed in June, though the season became active in July when five named storms developed, including Hurricane Daniel which was the second strongest storm of the season, as well as Tropical Storm Emilia. During August, Hurricanes Ioke and John formed, as well as four other storms. September was a relatively quiet month with two storms, of which one was Hurricane Lane. Three storms developed in October including Hurricane Paul and two formed in November; this marked the second time on record, after 1961, when more than one tropical storm developed in the basin during the month of November. Damage across the basin reached $355.1 million (2006 USD), while 14 people were killed by the various storms.
|May 22, 2006
|Actual activity
On May 22, 2006, the National Oceanic and Atmospheric Administration's (NOAA) CPC (CPC) released their forecasts for the 2006 Atlantic and Pacific hurricane seasons. The Pacific season was expected to be hindered by the decades-long cycle that began in 1995, which generally increased wind shear across the basin. NOAA predicted a below-normal level of activity in the Eastern Pacific, with 12–16 named storms, of which 6–8 were expected to become hurricanes, and 1–3 expected to become major hurricanes.[3] The Central Pacific Hurricane Center's area of responsibility was also expected to be below average, with only two to three tropical cyclones expected to form or cross into the area.[4] They expected that neither El Niño nor La Niña would affect conditions significantly.[3]
On May 15, the hurricane season began in the Eastern Pacific basin, which is the area of the northern Pacific Ocean east of 140°W.[5] On June 1, the season began in the Central Pacific warning zone (between 140°W and the International Dateline); however, no storms occurred in the region until July.[6]
The Accumulated Cyclone Energy (ACE) index for the 2006 Pacific hurricane season in total is 156.99 units (120.48 units in the Eastern Pacific and 36.513 units in the Central Pacific).[nb 1] Broadly speaking, ACE is a measure of the power of a tropical or subtropical storm multiplied by the length of time it existed. Therefore, a storm with a longer duration, such as Hurricane Ioke, which arrived with a total of 32.2250 units and then crossed to the Western Pacific, will have high values of ACE. It is only calculated for full advisories on specific tropical and subtropical systems reaching or exceeding wind speeds of 39 mph (63 km/h).
|Most intense Pacific hurricanes[7]
|Listing is only for tropical cyclones in the Pacific Ocean
north of the equator and east of the International Dateline
Overall, there were 19 tropical storms. In addition, 11 hurricanes developed. Furthermore, there were total of six major hurricanes, Category 3 or greater on the Saffir-Simpson Hurricane Wind Scale. The season officially started on May 15 in the East Pacific Ocean, and on June 1 in the Central Pacific; they both ended on November 30. No tropical storms developed in June in the basin, which was unusual compared to the average of two storms forming during the month.
From 1966 to 2008, there have been only three other seasons in which a tropical storm did not form in June, these being 1969, 2004, 2007 seasons.[8] After such an inactive month, the tropics became active in July when five named storms developed, including Hurricane Daniel which was the second strongest storm of the season. During August, Hurricanes Ioke and John formed, as well as four other storms. September was a relatively quiet month with two storms, of which one was Hurricane Lane.[7] By that time, however, El Niño conditions became established across the Pacific,[9] which is known to enhance Pacific hurricane activity.[3]
Three storms developed in October, including Hurricane Paul.[7] Tropical activity within the basin in November 2006 was the most active on record, based on the ACE Index. Three tropical cyclones formed, of which two became tropical storms; only one other season on record at the time, 1961, produced two tropical storms in the month of November.[10] In addition, Mexico was struck by four tropical cyclones in 2006, none on the Atlantic coast and all along the Pacific coast.[11] One hit Baja California Peninsula while the others made landfall on the mainland.[12]
An extratropical storm persisted in the extreme northern central Pacific Ocean in late October. It drifted over unusually warm waters up to 3.6 °F (2 °C) above normal, and gradually developed convection near the center. By November 2, QuikSCAT satellite suggested the system attained winds of up to 60 mph (95 km/h) about 900 mi (1450 km) west of Oregon. The system also developed an eye and an eyewall. The cyclone tracked northeastward as it gradually weakened, and dissipated on November 4. NASA considered the cyclone to be a subtropical storm. However, as it formed outside of the territory of any monitoring organization, it was not named. Operationally, the United States Navy treated the system as a tropical disturbance, numbered 91C.[13]
|Tropical storm (SSHWS)
|May 27 – May 30
|Peak intensity
|45 mph (75 km/h) (1-min) 1002 mbar (hPa)
The first storm of the year had its genesis from a tropical wave that crossed Central America and entered the East Pacific on May 21. The system interacted with a trough near the Gulf of Tehuantepec, causing thunderstorms to increase. A large low pressure area formed on May 25 south of Mexico, which organized slowly due to wind shear in the region. Early on May 27, the NHC designated the system as Tropical Depression One-E about 190 mi (305 km) south of Acapulco.[14] The nascent storm moved little, and the wind shear displaced the center west of the convection.[15] Late on May 27, the NHC upgraded the depression to Tropical Storm Aletta.[14] While named tropical cyclones in May are infrequent events, Aletta marked the seventh consecutive year to have a named cyclone form in May.[16] The storm drifted for several days off the southern coast of Mexico. The NHC estimated peak winds of 45 mph (75 km/h) on May 28,[14] as the storm presented an elongated cloud structure.[17] Increased wind shear and dry air caused weakening on May 29, and Aletta weakened into a tropical depression. Drifting westward, the system became a remnant low on May 31, and dissipated soon afterward.[14]
The storm moved toward the Guerrero coast in southwestern Mexico, prompting the Mexican government to issue tropical storm watches between Punta Maldonado and Zihuatanejo.[18] Aletta produced moderate rainfall across Mexico, including a 24-hour rainfall total of 100 mm (3.94 inches)[nb 2] in Jacatepec, Oaxaca on May 30, and 96 mm (3.78 inches) in La Calera, Guerrero, on the next day.[18] High winds knocked down trees and caused minor structural damage. In Zihuatanejo, a ship with nine people was rescued after being reported as lost, which may have been a result of high seas generated by Aletta.[19]
|Tropical depression (SSHWS)
|June 3 – June 5
|Peak intensity
|35 mph (55 km/h) (1-min) 1005 mbar (hPa)
On the day after Aletta dissipated, a new area of disturbed weather developed off the southwest Mexican coast. High shear slowed the development of the system, although it gained enough convection and organization to be classified as a tropical depression on June 3. The depression strengthened to near tropical storm status as it approached the coast of southwestern Mexico; however, shear persisted over the system and it weakened before dissipating on June 4.[20]
Despite never becoming a named storm, heavy rain occurred, including a total of 19.13 inches (486 mm) measured in a 48‑hour period in Acapulco.[21] Mudslides and flash flooding were reported,[20] forcing 72 people from their homes.[22] No deaths or serious damage was reported.[20]
|Category 3 hurricane (SSHWS)
|July 11 – July 16
|Peak intensity
|125 mph (205 km/h) (1-min) 953 mbar (hPa)
A tropical wave exited the west coast of Africa on June 27, which reached the eastern Pacific on July 7. The system spawned a low pressure area south of Mexico. Associated convection gradually became better organized, and the system organized into Tropical Depression Three-E early on July 11. Steered by a subtropical ridge over Mexico, the storm tracked west-northwestward for its entirety. Located over warm waters, the depression intensified into Tropical Storm Bud within six hours of its formation.[23] The thunderstorms organized, with good outflow except to the east due to the presence of Tropical Storm Carlotta. On July 12, the NHC upgraded Bud to a hurricane, after an eye developed in the storm's center.[24][23][25] Later on July 12, Bud was upgraded to a Category 2 hurricane on the Saffir-Simpson Hurricane Scale.[23]
Early on July 13, Bud became a Category 3 hurricane, or a major hurricane. At that time, the well-defined eye was enclosed by a ring of deep thunderstorms.[26] That day, the hurricane reached its peak intensity of 125 mph (205 km/h) and a minimum barometric pressure of 953 mbar (28.1 inHg). Bud encountered cooler waters and stable air, and a period of rapid weakening began.[23] The eye became obscured, and core convective cloud tops began to warm,[27] until much of the convection was lost on July 14, impeded by southeasterly wind shear.[23] On July 15, Bud was downgraded to a tropical depression, and the next day it degenerated into a remnant low . The low fully dissipated on July 17 about 750 mi (1,210 km) east-northeast of Hawaii.[23] The remnants of Bud produced light rainfall across Hawaii.[28]
|Category 1 hurricane (SSHWS)
|July 12 – July 16
|Peak intensity
|85 mph (140 km/h) (1-min) 981 mbar (hPa)
A tropical wave exited Africa on June 30 and moved across the Atlantic Ocean without development. On July 9, while crossing Central America into the eastern North Pacific Ocean, thunderstorm activity increased, and the system organized into Tropical Depression Four-E early on July 12 about 290 mi (465 km) south of Zihuatanejo, Guerrero.[29] The large depression moved quickly to the west-northwest to the south of a ridge over northwestern Mexico, and its outer rainbands moved across the coast. Rainfall totals were less than 1 inch (25 mm).[29] The depression intensified into Tropical Storm Carlotta just six hours after forming.[29] By late on July 12, the storm developed banding features,[30] and early on July 13 Carlotta attained hurricane status about 430 mi (700 km) south of the southern tip of the Baja California peninsula.[29]
As Carlotta intensified, the system became more compact, and it reached peak winds of 85 mph (140 km/h) on July 13.[29] An eye formed in the center, and the hurricane was briefly forecast to attain major hurricane status, or a Category 3 on the Saffir-Simpson scale.[31] However, Carlotta weakened due to increased wind shear from Hurricane Bud to its west,[29] and the eye and convection deteriorated.[32] Carlotta briefly weakened to tropical storm status late on July 14, although a decrease in shear allowed it to reintensify into a hurricane. This was short-lived as the center moved into the area of cooler waters, and Carlotta again weakened to tropical storm status.[29] Late on July 15, the circulation became separated from the convection,[33] and Carlotta weakened to tropical depression status on July 16, and the next day generated into a remnant low. The circulation continued generally westward, dissipating on July 20 about 1500 mi (2400 km) east of the Hawaiian islands.[29]
|Category 4 hurricane (SSHWS)
|July 16 – July 26
|Peak intensity
|150 mph (240 km/h) (1-min) 933 mbar (hPa)
On July 16, a tropical disturbance formed far to the south of the Baja California Peninsula and quickly increased in convective activity and organization, becoming a tropical depression. The system continued to organize and was designated as a tropical storm the next day. On July 18, Daniel attained hurricane status, and two days later underwent rapid intensification; it reached major hurricane status and was later upgraded further to Category 4 status on the Saffir-Simpson Hurricane Scale. Its peak intensity was 150 mph (240 km/h).[34] The hurricane underwent eyewall replacement cycles, which are internal mechanisms that occur in most intense hurricanes. Daniel later became an annular hurricane, which allowed it to maintain Category 4 status for longer than it otherwise would have.[35]
It crossed over into the Central Pacific early on July 24 and was predicted to affect Hawaii as a tropical storm; however, Daniel encountered weak steering currents in the open ocean, causing it to slow down considerably.[34] It rapidly degenerated to a tropical depression on July 25, and the CPHC issued its last advisory on July 26 while the storm was still well to the east of Hawaii. Its remnants later moved across the Hawaiian islands,[34] dropping heavy rainfall and causing flooding.[9] West Wailuaiki on Maui recorded 3.87 inches (98 mm) in one day, which was the highest daily rainfall total from the hurricane.[28]
|Tropical storm (SSHWS)
|July 21 – July 28
|Peak intensity
|65 mph (100 km/h) (1-min) 990 mbar (hPa)
The origins of Emilia were from a tropical wave that developed into a tropical depression on July 21, a short distance off the coast of Acapulco. It moved generally north-northwestward, reaching tropical storm status on July 22 and passing about 175 mi (280 km) southwest of Manzanillo, Colima.[36] An eyewall began to form that day,[37] and Emilia reached peak winds of 65 mph (105 km/h).[36] It briefly weakened due to wind shear, although restrengthening occurred as the storm turned toward the Baja California peninsula. On July 26, Emilia again reached peak winds of 65 mph (105 km/h), and shortly thereafter it passed about 60 mi (95 km) southwest of the southern tip of Baja California. It weakened as it turned into cooler waters, first to tropical depression status on July 27 and then to a convective-less remnant low on July 28. The remnants dissipated on July 31 about 495 mi (800 km) west-southwest of San Diego, California.[36]
In southwestern Mexico, Emilia produced tropical storm force winds along the coastline. Rainfall in the southern portion of the Baja California peninsula caused minor flooding, and gusty winds caused damage to buildings and power lines.[36] Moisture from Emilia reached the southwestern United States. Thunderstorms and rainfall occurred across Arizona, causing flooding.[38] In southern California, the storm dropped light rainfall, which assisted firefighters in containing a wildfire.[39]
|Tropical storm (SSHWS)
|July 31 – August 3
|Peak intensity
|50 mph (85 km/h) (1-min) 1000 mbar (hPa)
A tropical wave crossed the west coast of Africa on July 15 and entered the Pacific on July 25. Convection increased on July 28, and at 1800 UTC on July 31 the system became Tropical Depression Seven-E about 980 miles (1,580 km) southwest of the southern tip of the Baja California peninsula. Six hours later, the depression was upgraded to Tropical Storm Fabio. It moved westward due to a ridge to its north, and on August 1 Fabio reached peak winds of 50 mph (85 km/h). Later, the storm began weakening due to increased wind shear and dry air. On August 3, Fabio deteriorated to tropical depression status, and later that day it degenerated into a remnant low pressure area. The remnants continued westward, moving across Hawaii on August 7.[40]
Although Fabio did not impact land, its remnants produced heavy rainfall in Hawaii. In a 24-hour period, 2.89 inches (73 mm) of rainfall was recorded at Glenwood on the island of Hawaii; this was the highest daily rainfall total for the month on the island. However, the heaviest precipitation fell on Mount Waiʻaleʻale on Kauai, where 15.08 inches (383 mm) fell in 24 hours; this total alone was greater than all other monthly rainfall totals in the state.[41] The heavy rainfall flooded the Hanalei River, which forced the closure of the Kuhio Highway when a bridge was inundated.[40] On Oahu, the rainfall caused ponding on roadways and flooding along streams. One flooded stream stranded 24 hikers along a trail, all of whom required rescue by helicopter.[42]
|Tropical storm (SSHWS)
|August 1 – August 3
|Peak intensity
|40 mph (65 km/h) (1-min) 1004 mbar (hPa)
On July 17, a tropical wave exited Africa and crossed the Atlantic without developing. On July 25 it entered the Eastern Pacific, gradually developing an area of organized convection. Despite marginally favorable upper-level winds, the system organized enough to be declared a tropical depression on August 1, several hundred miles southwest of Acapulco, Mexico.[43] Initially, the depression tracked west-northwestward.[7] Despite wind shear in the area,[44] the depression was upgraded to Tropical Storm Gilma later on August 1. The wind shear prevented further strengthening or organization, and Gilma weakened to a tropical depression early on August 2.[43] The depression turned westward,[7] and Gilma degenerated into a remnant low by August 4.[43]
|Category 2 hurricane (SSHWS)
|August 15 – August 23
|Peak intensity
|110 mph (175 km/h) (1-min) 966 mbar (hPa)
A tropical wave exited Africa on July 31, and after no development in the Atlantic, it crossed Central America into the northeastern Pacific Ocean on August 10. Convection gradually increased, and a broad low pressure area developed about 375 miles (605 km) south of Acapulco, Mexico on August 13. The system continued to become organized, and it developed into a tropical depression around 1800 UTC on August 15 about 650 mi (1,045 km) south-southwest of the southern tip of Baja California. It moved west-northwestward, located south of a ridge that extended westward from northern Mexico westward into the Pacific. The depression quickly intensified into Tropical Storm Hector early on August 16.[45] Hector was able to steadily strengthen, reaching hurricane status at 0600 UTC on August 17. It is estimated that Hector reached its peak intensity of 110 mph (175 km/h) at 0600 UTC on August 18, while centered about 1,035 mi (1,665 km) southwest of the southern tip of Baja California.[7]
Hector remained a Category 2 hurricane for about 24 hours.[7] Shortly thereafter, it encountered cooler waters and westerly shear,[46] and Hector steadily weakened until becoming a tropical storm by August 20. Shortly thereafter, the storm reached a weakness in the subtropical ridge, which caused it to move slowly to the northwest. By August 21, deep convection was confined to the northeast portion of the circulation.[47] The shear was not strong enough to completely weaken the tropical cyclone and Hector remained a tropical storm with 50 mph (85 km/h) winds for about 24 hours.[45] After the remaining shower and thunderstorm activity dissipated on August 22, the cyclone turned westward in response to the low-level easterly wind flow.[48] Hector weakened to a tropical depression at 0000 UTC on August 23, and to a remnant low six hours later. The remnant circulation of Hector dissipated on August 24 about 750 mi (1,210 km) east of the Hawaiian Islands.[49]
|Category 5 hurricane (SSHWS)
|August 20 – August 27 (Exited basin)
|Peak intensity
|160 mph (260 km/h) (1-min) 915 mbar (hPa)
The cyclone developed from the Intertropical Convergence Zone on August 20 far to the south of Hawaii. Encountering warm waters, little wind shear, and well-defined outflow, Ioke intensified from a tropical depression to Category 4 status within 48 hours. Late on August 22 it rapidly weakened to Category 2 status before crossing over Johnston Atoll. Two days later favorable conditions again allowed for rapid strengthening, and Ioke attained Category 5 status on August 25 before crossing the International Date Line. At the time, its barometric pressure was estimated at 915 mbar, thus becoming the strongest hurricane on record in the Central Pacific.[9] As it continued westward its intensity fluctuated, and on August 31 it passed near Wake Island with winds of 155 mph (249 km/h). Ioke gradually weakened as it turned northwestward and northward, and by September 6 it had transitioned into an extratropical cyclone.[50] By then, the cyclone had lasted 19 days, reaching the equivalent of Category 5 status on the Saffir-Simpson Hurricane Scale three times.[9] The remnants of Ioke accelerated northeastward and ultimately crossed into Alaska.[51]
Ioke did not affect any permanently populated areas in the Central Pacific or Western Pacific basins as a hurricane or a typhoon. A crew of 12 people stayed in a hurricane-proof bunker on Johnston Atoll during the hurricane's passage; the crew estimated winds reached over 100 mph (160 km/h), which damaged trees on the island but did not impact the island's bird population.[9][52] The hurricane left moderate damage on Wake Island totaling $88 million (2006 USD), which resulted from blown off roofs and damaged buildings, although the infrastructure of the island was left intact. All military personnel were evacuated from the island, the first full-scale evacuation of the island since Typhoon Sarah in 1967.[53][54][55] Later, the extratropical remnants of Ioke produced a severe storm surge along the Alaskan coastline, causing beach erosion.[56]
|Category 3 hurricane (SSHWS)
|August 21 – August 27
|Peak intensity
|120 mph (195 km/h) (1-min) 955 mbar (hPa)
A tropical wave exited the west coast of Africa on August 8, and entered the eastern Pacific on August 16. Three days later, a weak low pressure area formed, and thunderstorms consolidated near that feature. On August 21, the NHC designated the system Tropical Depression Ten-E about 350 mi (560 km) south-southwest of Acapulco, Mexico. A ridge over Mexico steered the system to the northwest through an area of warm waters and low wind shear. With favorable conditions, the depression quickly intensified into Tropical Storm Ileana.[57] An eye formed in the center of the convection, and Ileana attained hurricane status late on August 22.[58] On August 23, about 48 hours after forming, Ileana reached major hurricane status and a peak intensity of 120 mph (195 km/h), with a minimum pressure of 955 mbar (28.2 inHg). At that time, the storm was about 60 mi (100 km) southeast of the unpopulated Socorro Island.[57] During the storm's passage nearby, a station on the island recorded sustained winds of 59 mph (95 km/h), with gusts to 77 mph (125 km/h).[57]
As Ileana was heading north along the Mexican coastline, slight rainfall was recorded along the coast,[59] which caused some flooding in Nayarit, Jalisco, Colima, Michoacán, and Baja California Sur.[60] High surf killed a man near Cabo San Lucas, despite warnings not to swim in the ocean.[61] Despite forecasts of further intensification to Category 4 status,[62] Ileana began weakening due to cooler waters. The thunderstorms waned, and the storm slowed its forward motion.[57][63] On August 26, Ileana weakened to tropical storm status as convection decreased markedly. The next day, the storm deteriorated to tropical depression status, and later a remnant low after being devoid of thunderstorms. The low continued slowly westward, dissipating on August 29 about 830 mi (1340 km) west-northwest of Cabo San Lucas.[57]
|Category 4 hurricane (SSHWS)
|August 28 – September 4
|Peak intensity
|130 mph (215 km/h) (1-min) 948 mbar (hPa)
On August 28, a persistent area of low pressure southwest of Acapulco, Mexico developed into a tropical depression. Later that day it strengthened into a tropical storm, and it reached hurricane strength 24 hours later on August 29. John underwent rapid intensification and reached Category 3 intensity later that day and Category 4 on August 30.[64] Hours later, the hurricane underwent another eyewall replacement cycle,[65] and subsequently weakened to Category 3 status as it paralleled the Mexican coastline a short distance offshore.[66] Potentially due to its eyewall replacement cycle or its interaction with land, John weakened to a 105 mph hurricane by late on August 31,[67] but restrengthened to a major hurricane shortly after. It made landfall near the southern tip of the Baja California peninsula as a Category 2 hurricane on September 1.[68] John continued northwestward along the eastern Baja California peninsula, weakening to tropical depression status by September 3 and dissipating on September 4 in the Gulf of California.[64]
Along the southwestern coast of Mexico, John produced heavy surf, strong winds, and heavy rainfall, which flooded roads, caused mudslides, and downed trees.[64][69] Along the Baja California Peninsula, the hurricane dropped heavy rainfall, with a 24-hour peak of 10.8 inches (276 mm) in Los Planes.[70] The heavy rainfall caused flooding, closed roads,[71] and caused a dam to overflow.[72] The winds and rainfall destroyed thousands of flimsy houses across the region.[73] Across Mexico, five people were killed,[64] and damage amounted to $663 million (2006 MXN, $60.8 million 2006 USD).[74] Moisture from the remnants of John produced flooding across Texas, which closed a ½ mile (800 m) portion of Interstate 10 in El Paso.[75] In southern New Mexico, the rainfall caused widespread street flooding and some minor damage.[76] Tropical moisture from the storm also produced rainfall in Arizona and southern California, where eight separate mudslides occurred, trapping 19 vehicles but causing no injuries.[77]
|Category 1 hurricane (SSHWS)
|August 30 – September 8
|Peak intensity
|80 mph (130 km/h) (1-min) 985 mbar (hPa)
On August 30, a tropical wave located about 525 miles (850 km) south-southwest of Baja California became more organized and was designated as the twelfth tropical depression of the 2006 season. It strengthened into Tropical Storm Kristy and became Hurricane Kristy the next day. It did not retain this status for long, partly due to its proximity to Hurricane John.[78] There was a possibility of a Fujiwhara interaction between both systems, causing Kristy to weaken or perhaps be absorbed into the circulation of John.[79] This did not occur, however. Kristy weakened steadily after its peak intensity and looked to be close to dissipating, but on September 3 and again on September 5, convection flared up and it returned to tropical storm strength.[78] After oscillating between storm and depression strength, the system degenerated into a remnant low on September 7, which dissipated on September 8 without affecting land.[78]
|Category 3 hurricane (SSHWS)
|September 13 – September 17
|Peak intensity
|125 mph (205 km/h) (1-min) 952 mbar (hPa)
On September 13, a tropical disturbance located about 125 miles (200 km) west-southwest of Acapulco, Mexico, gradually became better organized and was designated the thirteenth tropical depression of the 2006 season. The depression intensified in a favorable environment, and was upgraded to Tropical Storm Lane later that night. As it moved parallel to the Mexican coast it continued to strengthen and became a hurricane on September 15, and a major hurricane early the next day. Hurricane Lane reached peak winds of 125 mph (205 km/h) before it made landfall on the coast of Sinaloa on September 16. It quickly weakened over land and dissipated on September 17.[80]
Tropical Storm Lane produced heavy rainfall and high seas along the west coast of Mexico, including Acapulco where flood waters reached 16 inches (40 cm) in depth. The Acapulco airport also experienced flooding, though service was not interrupted.[81] Throughout Mexico, the hurricane caused four deaths and $2.2 billion (2006 MXN, $203 million 2006 USD) in damage,[82] half of which in Sinaloa where heavy crop damage was reported.[83] An estimated 4,320 homes were affected by the hurricane, and 19,200 miles (30,000 km) of roads and highways were damaged to some degree, including some destroyed bridges.[82]
|Tropical storm (SSHWS)
|September 16 – September 18
|Peak intensity
|45 mph (75 km/h) (1-min) 999 mbar (hPa)
A disturbance associated with a northerly extension of the Intertropical Convergence Zone and a tropical wave developed a closed circulation on September 15. It moved northeastward due to the influence from nearby Hurricane Lane, and organized enough to be declared Tropical Depression Fourteen-E on September 16 while located about 500 miles southwest of Cabo San Lucas, Mexico. It quickly strengthened, and organized into Tropical Storm Miriam later that day. After reaching a peak intensity of 45 mph (70 km/h), vertical wind shear and cooler waters rapidly weakened the storm, and the circulation decoupled from the convection on September 17. After turning more towards the north, Miriam weakened to tropical depression status, and on September 18 it degenerated to a remnant low. The remnant circulation turned to the northwest, then to the east, and dissipated on September 21 a short distance west of Baja California. No deaths are damage are associated with Miriam, and only one ship recorded winds of over tropical storm force near the center.[84]
|Tropical depression (SSHWS)
|September 19 – September 20
|Peak intensity
|35 mph (55 km/h) (1-min) 1007 mbar (hPa)
On September 19, an area of disturbed weather associated with the Intertropical Convergence Zone became sufficiently organized to be designated Tropical Depression Two-C. Initially, it was thought that the depression formed from the remnants of Hurricane Kristy, although subsequent analysis confirmed they were two separate systems. Initially, the depression was in an area of favorable conditions, with little wind shear and warm waters.[9] As a result, the CPHC predicted significant strengthening to at least hurricane status.[85] Instead, a high pressure system to its north increased wind shear over the depression, causing the convection to become removed from the center. The depression weakened into a remnant low on September 20, never reaching tropical storm status.[9]
|Tropical depression (SSHWS)
|September 26 – September 27
|Peak intensity
|35 mph (55 km/h) (1-min) 1005 mbar (hPa)
During September, El Niño conditions became established across the Pacific, which produced an area of warmer waters along the International Date Line. A few days after Tropical Depression Two-C dissipated, another area of disturbed weather formed, and although it was disorganized, it was also persistent. The CPHC initiated advisories on Tropical Depression Three-C on September 26 after a circulation was evident in the system. Strong wind shear prevented any development, and the system dissipated on September 27.[9]
|Tropical storm (SSHWS)
|October 9 – October 15
|Peak intensity
|50 mph (85 km/h) (1-min) 1000 mbar (hPa)
Early in October, a low pressure system began to organize to the west of the Mexican coast, and on October 9 it developed into Tropical Depression Fifteen-E. It strengthened into a tropical storm the next day, but strong wind shear and low sea-surface temperatures hindered development. Norman slowly began to weaken, and on October 11 it degenerated into a remnant low pressure area. Turning eastward, the system combined with a new tropical disturbance off the southwest Mexican coast, and slowly began to reorganize. The system was re-designated a tropical depression on October 15 just south-southeast of Manzanillo, Colima, although within a few hours it again dissipated.[86]
The storm brought heavy rainfall to southwestern Mexico, peaking at 6.35 inches (161 mm) in La Villita, Michoacán.[87] The rainfall caused flooding and mudslides around Acapulco, affecting 170 homes, of which 20 were destroyed.[88][89] About 300 hectares (740 acres) of crop fields sustained damage.[89] Initially there were two people missing;[89] however, a subsequent report indicated there were no casualties associated with the storm.[86]
|Tropical storm (SSHWS)
|October 9 – October 12
|Peak intensity
|45 mph (75 km/h) (1-min) 1000 mbar (hPa)
On September 18, a tropical wave exited Africa and later crossed into the eastern Pacific on September 29 without development. Convection increased in the Pacific along the wave axis, spawning a broad low pressure area on October 5. Despite the presence of wind shear, it organized enough for the NHC to initiate advisories on Tropical Depression Sixteen-E on October 9 about 1,360 miles (2,190 km) to the west-southwest of the southern tip of Baja California.[90] Influenced by a high pressure system, the depression drifted northward.[91] Six hours after being upgraded to a tropical storm, Olivia attained peak winds of 45 mph (75 km/h),[90] although the convection was limited to its northern side due to wind shear.[92] On October 11, the convective activity diminished and Olivia weakened to tropical depression status.[93] Olivia deteriorated into a remnant low on October 13. It moved towards the east-southeast, and on October 15 was absorbed into the remnants of Tropical Storm Norman. Olivia never affected land.[90]
|Tropical depression (SSHWS)
|October 13 – October 14
|Peak intensity
|35 mph (55 km/h) (1-min) 1007 mbar (hPa)
In the middle of October, the Intertropical Convergence Zone extended across the central Pacific Ocean, resembling an extension of the monsoon trough. An area of disturbed weather formed well to the southwest of Hawaii, organizing slowly for several days. Late on October 13, after the development of a low-level circulation and persistent convection, the CPHC classified the system as Tropical Depression Four-C about 750 mi (1,200 km) southwest of Honolulu, Hawaii. Upon being classified, the depression was located in an unusual steering flow that caused it to track eastward. Due to the approach of an upper-level trough, it was expected to dissipate quickly from wind shear, although forecasters noted the possibility for the trough to provide an outflow channel, which might allow strengthening.[94] On October 14, strong wind shear removed the convection completely from the center, and the system degenerated into a remnant low.[9]
The remnant circulation continued slowly eastward, dissipating on October 16. Concurrently, the convection tracked northeastward ahead of the upper-level trough, which contributed to heavy rainfall and flooding on the island of Hawaii on October 17.[9] The rainfall event coincided with the 2006 Kiholo Bay earthquake striking the area.[95]
|Category 2 hurricane (SSHWS)
|October 21 – October 26
|Peak intensity
|105 mph (165 km/h) (1-min) 970 mbar (hPa)
Hurricane Paul developed from an area of disturbed weather on October 21, and slowly intensified as it moved into an area of warm waters and progressively decreasing wind shear. Paul attained hurricane status on October 23, and later that day it reached its peak intensity of 105 mph (165 km/h), a strong Category 2 hurricane on the Saffir-Simpson scale. A strong trough turned the hurricane to the north and northeast into an area of strong vertical shear, and Paul weakened to a tropical storm on October 24, later passing just south of the Baja California Peninsula. Paul weakened to a tropical depression on October 25 a short distance off the coast of Mexico, and after briefly turning away from the coast it made landfall on northwestern Sinaloa on October 26.[96]
Paul was the third hurricane to threaten western Mexico in the season, the others being Hurricanes John and Lane. Rough surf killed two people along Baja California Sur,[97] while two deaths from flooding were reported in Sinaloa.[98] Paul dropped moderate rainfall across mainland Mexico, including a 24-hour total of 2.28 inches (58 mm) in Mazatlán, Sinaloa.[99] Damage totaled more than $35 million (2006 MXN, $3.2 million 2006 USD).[100]
|Tropical depression (SSHWS)
|October 26 – October 27
|Peak intensity
|35 mph (55 km/h) (1-min) 1007 mbar (hPa)
The origins of Tropical Depression Eighteen-E were from a tropical wave that exited the coast of Africa on October 7. It briefly spawned a low-pressure area as the wave continued westward without development. On October 20, the wave entered the Pacific Ocean, developing an area of thunderstorms about four days later. By 1200 UTC on October 26, a tropical depression formed about 155 mi (260 km) south of Manzanillo.[101] Initially, Tropical Depression Eighteen-E was located in an area of light wind shear, and the NHC anticipated further organization and strengthening to near hurricane status.[102] The tropical depression initially maintained a steady westward motion away from the Mexican coastline, due to a ridge north of the cyclone.[102] By October 17, convection had decreased, and the depression was not forecast to intensify as much.[103] Possibly due to intrusion of dry air, the circulation became exposed from the thunderstorms, and having weakened, it turned to a southward drift.[104] By 0000 UTC on October 28, the system had weakened to a non-convective remnant low, which dissipated the following day.[101]
|Tropical storm (SSHWS)
|November 8 – November 10
|Peak intensity
|40 mph (65 km/h) (1-min) 1002 mbar (hPa)
A tropical wave exited western Africa on October 22 and continued westward into the Pacific on November 2, spawning a tropical depression on November 8 about 440 mi (710 km) south of Manzanillo, Colima.[105] Environmental conditions appeared favorable,[106] although wind shear removed the convection from the circulation.[107] Throughout its duration, the storm maintained a northwest track through a weakness in a subtropical ridge.[108] By November 9, a new area of convection persisted near the center,[109] and a banding feature formed.[108] Despite the shear, the depression was upgraded to Tropical Storm Rosa, although the shear prevented intensification beyond its peak of 40 mph (65 km/h).[105] Rosa remained a tropical storm for only 18 hours, becoming a tropical depression early on November 10 and dissipating later that day.[105] Rosa was the first tropical storm in the basin to develop during November since 2000, and was also the first tropical depression to form in the month since 2002's Tropical Depression Sixteen-E. No impact was reported from the storm.[105]
|Tropical depression (SSHWS)
|November 11 – November 11
|Peak intensity
|35 mph (55 km/h) (1-min) 1007 mbar (hPa)
A tropical wave moved off the western coast of Africa on October 21, briefly developing two weak low pressure areas before the wave crossed into the Pacific Ocean on November 1. Thunderstorm activity slowly increased as the wave interacted within the Intertropical Convergence Zone. After a curved band of convection developed, it is estimated the system formed into Tropical Depression Twenty-E around 0000 UTC on November 11, about 550 mi (1,050 km) southwest of Manzanillo. Throughout its duration, the depression never completely separated from the Intertropical Convergence Zone.[110] When the NHC issued its first advisory on the depression, the agency predicted slight intensification to tropical storm status and for the depression to last at least two days. This was due to a forecast of gradually increasing wind shear after the first 24 hours.[111] Instead, the circulation became very elongated; it is estimated the cyclone degenerated into a trough by late on November 11.[110]
|Category 2 hurricane (SSHWS)
|November 13 – November 20
|Peak intensity
|110 mph (175 km/h) (1-min) 965 mbar (hPa)
Just days after Tropical Depression Twenty-E degenerated into an open trough, Tropical Depression Twenty One-E developed from a tropical wave on November 13 about 460 miles (740 km) south of Manzanillo, Colima. It steadily intensified as it tracked southeastward, reaching peak winds of 110 mph (175 km/h) on November 15. Subsequently, it began to weaken due to increased wind shear as it turned to the north. Sergio later turned to the west, remaining well off the coast of Mexico, and it dissipated on November 20 about 320 miles (515 km) west-northwest of where it originally formed.[112]
Sergio produced light rainfall along the coast of Mexico, though its effects were minimal.[113] The formation of Sergio marked the 2006 season as the most active in 12 years and the second season in which more than one tropical storm formed in November, after 1961. Sergio set records for the month of November in the basin. At the time, it was considered the strongest hurricane to form in the month; although it has since dropped to third after Sandra from 2015, and Kenneth from 2011. It is however, still considered the longest-lived November Pacific tropical cyclone with a duration of seven days.[1][112]
On October 28, 2006, a cut-off extratropical cyclone stalled over the northeast Pacific Ocean and began to strengthen. By October 31, the storm had acquired tropical characteristics, including an eye, convection, and a warmer-than-average core.[114] The system reached peak intensity on November 1, before slowly weakening and looping towards the Pacific Northwest. The system made landfall in Washington State on November 3, before rapidly weakening and dissipating on the next day. During the duration of the storm, the system was known as Storm 91C (or INVEST 91C). The storm's true nature still remains controversial among meteorologists today, due to disputes over the storm's exact structure and whether or not it had obtained tropical or subtropical characteristics.[115] Because the storm was not within the area of responsibility of the National Hurricane Center or the Central Pacific Hurricane Center, the storm was never assigned a name.
The following names were used for named storms that formed in the northeast Pacific in 2006.[116] This is the same list that was used in the 2000 season. There were no names retired from the northeast Pacific list. Therefore, the same list was reused in the 2012 season.
For storms that form in the Central Pacific Hurricane Center's area of responsibility, encompassing the area between 140 degrees west and the International Date Line, all names are used in a series of four rotating lists. The next four names that were slated for use in 2006 are shown below, however only the name Ioke was used.
The name Ioke was retired from the north-central Pacific list by the World Meteorological Organization in the spring of 2007 and replaced with Iopa.[117] During the 61st Interdepartmental Hurricane Conference, the Hawaii State Civil Defense requested the retirement of the name Daniel, citing that the storm had become memorable due to threat of damage.[118] However, the request was denied, as the name remains on the tropical cyclone naming list.[116]
This is a table of all the storms that formed in the 2006 Pacific hurricane season. It includes their duration, names, landfall(s), denoted in parentheses, damages, and death totals. Deaths in parentheses are additional and indirect (an example of an indirect death would be a traffic accident), but were still related to that storm. Damage and deaths include totals while the storm was extratropical, a wave, or a low, and all the damage figures are in 2006 USD.
|Dates active
|Storm category
at peak intensity
|Max 1-min
mph (km/h)
|Areas affected
|May 27 – 30
|Tropical storm
|45 (75)
|June 3 – 5
|Tropical depression
|35 (55)
|Southwestern Mexico, Western Mexico
|July 11 – 16
|Category 3 hurricane
|125 (205)
|July 12 – 16
|Category 1 hurricane
|85 (140)
|July 16 – 26
|Category 4 hurricane
|150 (240)
|July 21 – 28
|Tropical storm
|65 (100)
|Southwestern Mexico, Western Mexico, Baja California Peninsula, Southwestern United States
|July 31 – August 3
|Tropical storm
|50 (85)
|August 1 – 3
|Tropical storm
|40 (65)
|August 15 – 23
|Category 2 hurricane
|110 (175)
|August 20 – 27,[nb 3]
|Category 5 hurricane
|160 (260)
|Johnston Atoll, Wake Island, Minamitorishima, Southern Alaska
|$88 million
|August 21 – 27
|Category 3 hurricane
|125 (205)
|Socorro Island
|August 28 – September 4
|Category 4 hurricane
|130 (215)
|Guerrero, Michoacán, Baja California Sur, Arizona, California, New Mexico, Texas
|$60.9 million
|August 30 – September 8
|Category 1 hurricane
|80 (130)
|September 13 – 17
|Category 3 hurricane
|125 (205)
|Southwestern Mexico, Western Mexico, Northwestern Mexico, Southwestern United States
|$203 million
|September 16 – 18
|Tropical storm
|45 (75)
|September 19 – 20
|Tropical depression
|35 (55)
|September 26 – 27
|Tropical depression
|35 (55)
|October 9 – 15
|Tropical storm
|50 (85)
|Southwestern Mexico,[nb 4] Western Mexico
|October 9 – 12
|Tropical storm
|45 (75)
|October 13 – 14
|Tropical depression
|35 (55)
|October 21 – 26
|Category 2 hurricane
|105 (165)
|Oaxaca, Guerrero, Baja California Sur, Sinaloa
|$3.2 million
|October 26 – 27
|Tropical depression
|35 (55)
|November 8 – 10
|Tropical storm
|40 (65)
|November 11
|Tropical depression
|35 (55)
|November 13 – 20
|Category 2 hurricane
|110 (175)
|Season Aggregates
|25 systems
|May 27 – November 20
|160 (260)
|$355 million


text:
12 Nanny Jobs Found
In Home Care Needed
Posted by Jeremy G. on 1/25/2020
- 20 miles away (Nevada City, CA)
- $15/hr
- 1 child
My wife works from home and we need a vibrant, energetic in home sitter for our 9 month old daughter. Hours would be 9-3pm daily (M-F).
After school care
Posted by Kelli B. on 1/20/2020
- 19 miles away (Rocklin, CA)
- $12–15/hr
- 2 children
I'm in need of a great nanny to pick up two great kids after school. Monday pick up is 1:20. Tuesday through Friday is 2:20 pickup. Both have soccer practice during 3-4 days a week. This would require someone who has a good driving record and dependable with taking to practice and coordinating... More
Seeking A Fun, Active And Outgoing PT...
Posted by Christina D. on 1/20/2020
- 19 miles away (Rocklin, CA)
- $15–17/hr
- 2 children
We are looking for a fun, reliable, responsible + organized PT after-school nanny for 2 boys (7 & 11 yo) in Rocklin. Must be: college-aged, responsible, patient, kind, OK w/errands/shopping, kids' meals + chore help, have own reliable car/insurance, non-smoker, able to drive the kids around,... More
Part-time Nanny - schedule varies/ avg 16...
Posted by Nichole R. on 1/16/2020
- 7 miles away (Auburn, CA)
- $15–20/hr
- 2 children
We have two girls ages 13 months and 3 years. Our schedules change week to week and we will provide the schedule 1-2 weeks in advance. Our older daughter goes to preschool and will occasionally need to be dropped off/picked up.
Posted by Amy W. on 1/15/2020
- 12 miles away (Garden Valley, CA)
- $10/hr
- 1 child
Light cleaning. Mainly spending time with my 19 month old son and tending to his needs. (Feeding, drinking, napping)
Afternoon Nanny for 3 kids
Posted by Tamara B. on 1/14/2020
- 24 miles away (Orangevale, CA)
- $18/hr
- 3 children
I am need of an afternoon nanny 3 - 4x /week. Ideally nanny would start at 1:00pm with my infant until 4:00pm and then pickup my 2 and 4 year old from school and then assist with after school activities, dinner and bedtime routine. I am flexible on exactly which dates but would like to establish a... More
2 girls Ruby & Goldy 3&1
Posted by Dustin R. on 1/9/2020
- 7 miles away (Auburn, CA)
- $15–20/hr
- 2 children
Looking for a good person. Nichole & Dustin (parents).
Nanny for 2 weeks
Posted by Alyssa M. on 1/8/2020
- 7 miles away (Auburn, CA)
- $11/hr
- 2 children
We are in need of a nanny to assist my grandmother with looking after our two children. A 5 month old baby boy and a 2.5 year old girl. It would be for 2 weeks while our current nanny is out of town.
Angel for 16 Month Baby boy
Posted by Ardavan A. on 1/7/2020
- 23 miles away (Folsom, CA)
- $12–15/hr
- 1 child
We are searching for a nanny for our baby. We need someone M-F full time for at least 1 year. We're smoke free family and no pets. We need to have someone with references and clear background. We Both work for State. so we want to make sure you will be stay for at least 1 year. send your resume... More
Part Time Nanny for Twins
Posted by Robyn L. on 1/2/2020
- 19 miles away (El Dorado Hills, CA)
- $12–15/hr
- 2 children
Hello Everyone, I am a single mom looking for someone to help watch my son and daughter, possibly starting in May or June 2020 when I go back to work. I work 3 days a week, Thursday-Saturday. Hours would be Thursday and Friday 8:30 -4:15 Saturday 11-4 pm Possible some extra hours during the week... More
PT nanny in Rocklin for two sweet kiddos
Posted by Stefani C. on 12/29/2019
- 19 miles away (Rocklin, CA)
- $17/hr
- 2 children
Our current nanny, that we love, is moving on to a different career path and we are in need of a new nanny. We are in Rocklin by Whitney High and have a 7 and 4 year old. The children are the number one priority so we are looking for someone that isn't afraid to play and engage the children.... More
Caregiver to help with 1 year old
Posted by Cody F. on 12/28/2019
- 20 miles away (Placerville, CA)
- $20/hr
- 1 child
Need help taking care of baby while wife recovers from medical issue. Monday thru Thursday all day. Possibly overnight at times. Non smokers and drug free environment

subset: commoncrawl


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No Smith, no chance: Paul Gallen's answer to Queensland's problem
With roughly six weeks remaining until State of Origin Game 1, Queensland appears to have a problem.
"They're out of troops," as aptly summed up by Mat Thompson.
A string of unfortunate events is undoubtedly giving Maroons coach Kevin Walters a headache on top of an obvious selection predicament.
Greg Inglis, last year's captain, announced his sudden retirement from the game earlier this month. Leadership contenders Daly Cherry-Evans has an injured ankle and Roosters skipper Jake Friend tore his bicep off the bone.
A lack of obvious leaders and a dearth of kicking options has fanned the flames of a spicy State of Origin storyline:
The return of the messiah. All hail Cameron Smith.
Paul Gallen is the opposite of a Queensland fan favourite and has an obvious answer to the question of whether he'd like to see Smith pull on a maroon jumper once more.
"Well, as a New South Welshman, I hope he doesn't" Gallen told David Morrow and Mat Thompson.
"He's still the best player in the game in my opinion, he's a class act,
"I think they need him to be honest, he's a big difference in why the Blues won last year,
"He's so dangerous out of dummy half, his kicking game is impeccable, his passing game, his timing around the ruck, he's the best in the game still,
"If they're a big chance of winning they need Cameron Smith."
Smith retired from representative footy last year after realising he could no longer back up after an Origin match to play for his club. Asked whether Smith would be prepared to jeopardise a potential Melbourne Storm premiership for a brief return to the glory of Origin, Gallen suspects the choice would be an easy one.
"Probably winning a premiership to finish off his time at Melbourne,
"He's won plenty of Origin series and he's won a couple of comps too but I think winning the premiership would be the ultimate for him,
"If he did win the premiership this year, maybe he would pull the pin – you never know, particularly because he's going to surpass the 400 game mark already."
The same question was asked of Gallen, whether he would return to the Blues and play origin once more if his state called on his service and his response was emphatic.
"No, I wouldn't, not at this stage, not where I'm at at the moment, no way," he said.
"It's too hard, you're playing a whole season in three games, it's a 6 or 8 week period – it's a whole season,
"You've got that 8 or 9 days in camp, it's in the paper every single day, it's like club football goes out the window and it's purely about NSW vs Queensland,
"Each one of those games is like a Grand Final, you have to get yourself up for that and then depending on the result, [it affects] how you go back to club level,
"If you win you go back on a high you perform that week no problem, but if you don't win, you've got to get yourself back up again three days later,
"On top of that, it's the hardest football in the world to play, it's fast, it's tough, every tackle you feel,
"There's no way I could come back and play State of Origin at this stage, no way."
Click PLAY to hear more from Paul Gallen:


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Bathroom Solutions for Pugs that are Refusing to be House Broken
Have you spent 40 minutes with your pug on a walk, waiting for it to go the bathroom and giving up in despair, to only have it go the bathroom once you bring it back inside? Our Pug Experts have seen this many times. Whether your pug was not trained to relieve itself on walks or it just has become too old and fussy we have the bathroom solutions for your pug. Pugs are incredibly friendly and loyal dogs; however, they can be extremely high maintenance especially when it comes to simple task like relieving themselves while on a walk. Pugs are great apartment dogs because they are well tempered and become very lethargic as they age. If taking your dog proves to be useless to relieve themselves consider these useful tips to help your pug no longer go the bathroom in your home.
Steps to Help with Bathroom Solutions to Prevent Your Pug from Going the Bathroom in Your Home
- The first step to your pugs bathroom solution is to go to your local home improvement store (Home Depot or Lowes), and purchase a 2 Feet x 5 Feet sod of grass. You will want to ask a sales person for a large plastic trash bag to put the rolled up sod in so it won't dirty your car or truck. They should provide this bag free of cost.
- Bring the sod of grass on your balcony or backyard. You will want to tear the bag length wise so you will have a barrier to place the sod of grass on to prevent the grass from sticking to the floor.
- Unroll the sod of grass on the plastic bag. You should have a brand new piece of grass that your pug will enjoy.
- Introduce your pug to the sod of grass. Your pug should immediately understand that the piece of grass is theirs.
- You should now feed your pug on the balcony or backyard near the grass, so when your pug finishes eating they will be near the grass to relieve themselves. When your pug is finished relieving itself, you should pick up the poo with a paper towel and flush it down your toilet.
Care and Maintenance of Your New Grass
You should water your grass about once every two days. We suggest using about half a gallon of water and evenly distributing the water among the grass. In hotter seasons you may have to use a full gallon every two days. You can expect your grass to last about 3 to 6 weeks with regular maintenance.
Removing Your Grass
After about 3 to 6 weeks it will be time to replace your grass. An easy way to remove your used sod of grass is to have a large trash bag handy. If the dirt is slightly damp it will be easier to roll back up. You should roll the used grass up like a sushi roll using the plastic bag under the grass to keep everything neatly together. A friend should hold the new trash bag open while you place the old rolled up grass in it. You will want to throw the grass away in an approved spot, like a trash can that is meant to remove organic debris.


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Dear Friend of Chez François
The most valuable contribution we can give to the world is ourself, our talents, our skills, our wisdom, and our truth. Never dim your essence to make others feel comfortable. Listen to that inner voice. Let it be louder than the noise. Comparing ourselves to others is to hijacking peace of mind. Live a life of choice. Time is free but priceless.
Youthfulness is not a time or place, but rather a state of mind and lifestyle. There is no manual for this self-discovery journey. Our experiences become stories to tell, while conversations become hearts to touch. Each day brings a blank canvas to paint invaluable growth possibilities. Wherever you are, be there fully while living a simpler life.
Most things we fear exist only in our minds. Never let your fears become more prominent than dreams. Make peace with the past and friends with your mind, and keep it open, flexible, and teachable. Each day presents a unique opportunity to be a positive difference-maker. Strive to make someone's day special. Life is truly not about you and me. It is about those we serve and lead. Wealth is what we take from the world. Worth is what we give back. Inspire people to go beyond what they believe possible. What one does to others, we do to ourselves.
So take chances, bet on yourself, empower others, and do not wait for the perfect timing to get started. Because right now is the oldest you have ever been and the youngest you will ever be.


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International Journal of Remote Sensing
Call for Papers for Special Issues
Special Issue Call for Papers
There are currently no active calls for submissions for upcoming Special Issues. To see recently published Special Issues from International Journal of Remote Sensing visit our Special Issues page here.
Submission guidelines
All submissions will be peer reviewed according to the International Journal of Remote Sensing (IJRS) guidelines. Submitted manuscripts should not have been published or be under review elsewhere.
Prospective authors should consult the Instructions for Authors page on the journal homepage for guidelines and information on paper formatting and submission.
Authors should submit manuscripts using the IJRS manuscript central system at https://mc.manuscriptcentral.com/tres. Please choose 'IJRS Special Issue Paper' from the 'Manuscript Type' picklist on the submission form, irrespective of the paper type (i.e. even if your paper would normally be classified as a Research Letter, Tech Note, Research Paper, or Review Article). Also, please enter the appropriate Special Issue name in the space provided on the submission form for the name of the Special Issue.
IJRS has no page charges, and also does not charge for printing in color, if scientifically necessary. Open access publication is also possible, though a fee is charged for this. Click here for more information about open access options.
Should you have any submission questions, please contact Catherine Murray, Administrator of IJRS at: firstname.lastname@example.com.


text:
Cat Johnson is a writer and content strategist covering co-working, collaboration, and community. Publications include Yes! Magazine, Utne Reader, GOOD, Shareable, Triple Pundit, Mother Jones, and Lifehacker.
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Location: ALL CAMPUSES, Jacksonville Beach, FL US 32250
On Wednesday nights we offer a worship experience for the 6th-12th grade students. It starts at 6:30pm and ends at 8:30pm.
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* We are not a Club ~ We are a Family.
* We are not about numbers. We have long back stopped counting the number of riders we have in our family. Now it is about the Quality of rider you are, the attitude you possess and if you can gel with our family. By saying this, we don't mean we are closed for new riders. But it will take some time for us to accommodate you into our house.
* Our mission is to promote love for riding with safety and have fun at the same time.
* No Admin - No Moderator - No President - No Head - No Founder ~ Every Member is Equal.
* Many of our members belong to various other biker clubs. We don't have any issue with that.
* No discrimination on bikes, Any bike above 150 CC is welcome to join us. we are not interested in separatism in any way. We are not interested in playing into any of the divisions that have cropped up in the motorcycling and motorcycling club world over the years.
* Though there is no hierarchy in the club, we expect you to respect our senior members.
~ You learn lot of other things other than biking, You learn life from the experience of our senior members.
* We make a day ride every fortnight, 2 days ride once every month, 3 days rides once every 3 months, 5 days ride once every 6 months & a 15 days ride once in a year
* Conditions to join our rides are :
~ Bike maintenance - If you are not maintaining your bike properly we don't ride with you.
~ Helmets / Full Gear - No Helmet, No Full protective Gear - No Ride! Safety First!
~ Treat us the right way we treat you. No ego. If you have ego pls don't show it to us - We love peace!
~ Ride your own bike. Pls do not at all expect to borrow a bike from our club members.
~ No form of Intoxication during the ride. We hv a zero tolerance policy on this issue.
~ Where ever we ride, we respect the locals. No form of disturbance or nuisance to others.
* Anyone can call for a ride. Any wolf free during the date can join the ride.
* Whatsapp & Groups help us keep in everyday touch, grow and strengthen our relationship.
* We go dutch & try to keep trip expenses as economic as possible.
~ We stay in budget places. Even though not luxurious and flashy, we make sure the place is hygienic.
* We start our rides early in the mornings and reach the day's destination by the evening. We don't ride in the dark.
* We are serious riders. We do not wear our leathers as fashion statements.
* We seriously reflect the values of brotherhood/sisterhood, biker camaraderie and of supporting the larger biker community as well as our local communities.
* We do not judge other clubs for any decisions they make. That's not what we're about. We respect all other clubs and their interests. We will do this by attending as many club events, rallies and party's as we're able to.
* We are ready to support and ride for any social cause that will be beneficial for the society.


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Tesla Robotics League
Join a Team
FIRST Tech Challenge teams consist of:
- 2 or more adult mentors
- 3-15 students in grades 7th - 12th.
Tesla's Community Based Teams
- 5937 Renaissance Robotics - Apopka, Homeschoolers/ASCE (spots available for 2019-20) contact
- 6090 Rockstar Robotics - Orlando, Walt Disney World Clubhouse Branch Boys & Girls Club (spots available for 2019-20) contact
- 8601 Godly Gears - South Apopka, New Journey Youth Center (spots available for 2019-20) contact
- 9930 Robo-Knights - Orlando near UCF, Central Florida Stem Conference (spots available for 2019-20) contact
- 9779 PIEaters - Orlando near College Park, Community/Neighborhood Team
- 12917 Error 404 - Windermere, Community/Neighborhood Team
- 14418 Constant Chaos - Orlando, Maker Effect Foundation (spots available for 2019-20) contact
- 15459 Tech Legacy - Orlando, Operation Reach Back
- 16247 Avalanche - Port Orange, Gracious Youth, Inc. (spots available for 2019-20) contact
- 16733 Gra-V Robotics - Orlando, Maker Effect Foundation (spots available for 2019-20) contact
Tesla's Private School Teams
Teams are generally limited to students attending the private school. Attending students can contact the coach at their school for information on joining the school team.
- Bishop Moore Catholic High School, Orlando - 15033 Bug Bytes
- Forest Lake Academy, Apopka - 11020 SKI, 13761 Grappler BeBop
- Foundation Academy, Winter Garden - 12273 Spacing Out, 17305 FA Maelstron
- Lake Highland Preparatory School, Orlando - 9277 Hazmat Robotics Explosives, 10650 Hazmat Robotics Biohazards
- Real Life Christian Academy, Clermont - 12739 Regressive
- Saint Paul Catholic School, Leesburg - 17340 Saint Paul Catholic School
Volunteers make up 99% of the FIRST workforce. Whether you have just a few hours, one day, a weekend to help, want to mentor a team, have technical or non-technical expertise, there is a volunteer role suited to your unique interest. Find information about FIRST programs, volunteer resources, opportunities, and more!
Volunteer at an Event
Mentor a Team
Want to work with a team? One day? Every week?
Would you like to present to all teams at one of our Tesla events?
Let us know the type of team you're looking to support and your availability and we will help you get in contact.
As a mentor or coach of a FIRST Tech Challenge team, you are, through the kids, the key ingredient in the success of your team. Your contribution to the success of FIRST programs and ultimately to the success of FIRST is immeasurable.
Tesla's Public School Teams
Make a Difference!
Teams are generally limited to students attending the public school. Attending students can contact the coach at their school for information on joining the school team.
- Orlando Science Schools, Orlando - 5070 NUTS, 6379 Clockwork Mania, 7579 RobotSakers, 15064 Java Jedi, 15065 Binary Bosses, 15067 Motherboard Maniacs, 15517 PAWS, 17288 Rubber Bandits
- University High School, Orlando - 3939 Bolts of Steel & 6327 Fetch
Click image to contact Tesla Robotics League.
Start a FIRST Tech Challenge Team
Other Program Levels
Sometimes there is not a FIRST Tech Challenge team that is a good fit or matches your schedule. Start a new team! It's easier than you think! No experience necessary and you are never alone!
FIRST LEGO League Juniors team for ages 4-10 years old.
FIRST LEGO League team for ages 9-14 years old.
FIRST Tech Challenge team for ages 12-18 years old.
FIRST Robotics Competition team for ages 14-18 years old.
Useful Links:
Official Sources:
Events and Teams in My Area - for all program levels
Statewide FIRST Tech Challenge website - www.flfirst.org
Unofficial Sources:
Unofficial local groups that strive to help facilitate team matchmaking and the creation of new teams:
FIRST Tech Challenge of Central Florida (grades 7th-12th, typically ages 12-18)
FIRST LEGO League of Central Florida (gardes 4th -8th, typically ages 9-14)
FIRST LEGO League Juniors of Central Florida (grades K-4th, typically ages 4*-10)
These groups are run by the students of one of our Tesla teams.
Contact US
Click here to try again.


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ArmA Scripting Tutorials: Scripting Explosive Barrels
I tried to do it once before but didn't like the outcome. This time it is good enough to share. So basically in Arma 3
ArmA Scripting Tutorials: Epic Armour Drop
Arma 3 has rather large and round cargo parachutes, which where not animated until recently, big thanks to The Most Venerable Order of Configuration, Lord Pettka.
ArmA Scripting Tutorials: Rounding The Pounding
I want to dedicate this post to something that has been bothering me for awhile. Why? Because it has really simple solution and yet for
ArmA Scripting Tutorials: addAction Quirks V2
Continuing with addAction quirks, the 8th element in addAction params array is the condition statement. It has to return true in order for your custom
ArmA Scripting Tutorials: Fly Like An E… Seagull!
I'm going to make this blog post a little bit special today. I kinda feel like bitching about how buggy Arma 3 is and especially
ArmA Scripting Tutorials: How To Draw Icon On Map
Today I'm going to show you how to draw an icon on the map and how to make it change with map zoom. For this
ArmA Scripting Tutorials: Triggers V3
This is third part in the trigger series (1, 2) I've started on this blog. A day ago I've discovered that triggers, contrary to the
ArmA Scripting Tutorials: Code Performance
You might have used it already, but Arma 3 has this pretty neat library function BIS_fnc_codePerformance designed by Karel Moricky. And since in Arma you
ArmA Extension: hash_id.dll
Well, I don't really know why I made this. It seemed like a good idea a few days ago, so I started investigating and it
ArmA Scripting Tutorials: One Man Tank Operation
I will probably get some hate for this post from Arma vets for messing with realism aspect of the game, but being able to drive


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Rev. Greggory L. Brown, M.Div. '80
Wednesday, April 20, 2016
Rev. Greggory L. Brown, M.Div. '80 What do you do? I am Senior Pastor at Miracles of Faith Community Church (ELCA). I am blessed to serve a wonderful and diverse community in East Oakland, CA, with loving support and practical services that include, uplift, and unify all of God's people. What's the best thingRead More


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Major Details For Buying Bride Online In The United Kingdom
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Sponsored by:
TUI Cruises appoints independent environmental advisory board
TUI Cruises has appointed an independent environmental advisory board. Following a meeting last month, the company set its green agenda through the board, which includes experts from science, shipping, and politics. Board: • Prof Stefan Gössling, scientist and [Read more...]
Bakke quits Havyard Group
Geir Johan Bakke and the Havyard board have agreed to terminate his employment. Bakke (pictured) has been employed by the beleaguered Havyard Group since 2001, has been CEO since 2004, and has been central to the development of [Read more...]
Kaufman promoted to Executive Vice President for Carnival Brands
Carnival Corp has made several appointments in senior executive positions. Anthony 'Tony' Kaufman has been promoted to executive vice president, professional services and chief financial officer of Carnival Corp's four business units - Princess Cruises, Holland America Line, [Read more...]
Havyard appoints new general manager
Lasse Stokkeland is to leave his position as general manager of Havyard Ship Technology (HST), with the result that the Board has appointed Erlend Hatleberg to replace him. CEO of Havyard Group (HGR) and chair of the board [Read more...]
Sommer to take over NCL
Norwegian Cruise Line (NCL) has made organisational changes, scheduled to be implemented following the launch of ''Norwegian Encore', the company's newest cruise ship. They include the appointment of Harry Sommer (pictured) as NCL's President and CEO. He will [Read more...]
Princess appoints Prag Shah to new role
Princess Cruises has appointed Prag (Pragnesh) Shah to the position of global head of experience and innovation operations. He will lead the continued activation and expansion of MedallionClass vacations, including digital and live immersive experiences across the cruise [Read more...]
Ungerer to head up MSC's luxury brand
MSC has announced that industry veteran Michael Ungerer has joined its cruises business as CEO of MSC's new luxury brand. Ungerer (pictured) joins MSC with over 30 years of senior management experience in cruising, as well as in [Read more...]
Deer steps up at Fred. Olsen
Fred. Olsen Cruise Lines has appointed Peter Deer as the new managing director, with effect from 1st September, 2019. He will replace Mike Rodwell, who will retire from Fred. Olsen on 31st August, 2019, after over 30 years [Read more...]
AIDA appoints digital expert
Marketing and digital expert, Alexander Ewig, is to join AIDA Cruises' management team on 1st September, 2019. He will be responsible for the entire brand communication, including direct sales and e-commerce. "One of the biggest growth phases in [Read more...]
Genting Hong Kong announces appointment of Mr Michael Goh as president of Dream Cruises
Genting Hong Kong Limited has announced the appointment of Michael Goh as the President of Dream Cruises and Head of International Sales for Genting Cruise Lines. Goh (pictured) will continue to be based in Singapore, reporting to Kent [Read more...]