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Observering the surface energy budget at Cabauw : A status report

Introduction Closing the surface energy budget (SEB) is one of the longest outstanding problems in micro-meteorology. At the earth’s surface the net radiation (QN), consisting of the budget of shortwave incoming (K), shortwave outgoing (K), longwave incoming (L) and longwave outgoing radiation (L), should be balanced by the transport of heat into the soil (G) and to the atmosphere in the form of sensible (H) and latent heat (LE):