Large scale surface heat fluxesThe heat flux through the ocean surface, Q, is the sum of the net radiation at the surface, the latent heat flux into the atmosphere, and the sensible heat flux into the atmosphere (all fluxes positive upwards). A review is presented of the geographical distribution of Q and its constituents, and the current accuracy of measuring Q by ground based measurements (both directly and by 'bulk formulae') is assessed. The relation of Q to changes of oceanic heat content, heat flux, and SST is examined and for each of these processes, the accuracy needed for Q is discussed. The needed accuracy for Q varies from process to process, varies geographically, and varies with the time and space scale considered.
Document ID
19850042408
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Sarachik, E. S. (Harvard University Cambridge, MA, United States)
Date Acquired
August 12, 2013
Publication Date
January 1, 1984
Subject Category
Oceanography
Meeting Information
Meeting: Large-scale oceanographic experiments and satellites