Titlebook: Large-Scale Oceanographic Experiments and Satellites; Catherine Gautier,Michèle Fieux Book 1984 D. Reidel Publishing Company, Dordrecht, H

chemoprevention

慢慢啃

Satellite Sea Surface Temperature Determination from Microwave and Infrared RadiometryST) estimation accuracies of 0.5–1.0 C, sufficient to map on a global scale the large-scale SST field and its anomaly with respect to climatological norm. In addition, these sensors provide data on the wind at the sea surface, vertically integrated water vapor and liquid water, rain rate, and atmosp

沐浴

Ocean Surface Wind Stressation. Much can be done to improve our knowledge through better collection of existing observations, deployment of properly instrumented drifting buoys, better calibration and collection of cloud motion vectors, increased scrutiny and development of analysis/forecast methods of surface data assimila

尋找

Wind Speed and Stress Over the Ocean: Scatterometer versus Surface Measurementsat observational burden. The SEASAT experience demonstrated that its scatterometer system, SASS, could do the job, but the following problems still exist:.It is argued that at this stage, the next likely scatterometers, on NROSS (KU-band similar to SEASAT) and certainly ERS-1 (C-band), will both req

公理

拱墻

Large Scale Surface Heat Fluxesheat flux into the atmosphere (all fluxes positive upwards). A review will be 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”) will be assessed..The relation of Q to chang

波動(dòng)

Surface Radiation Budgetr climate studies. The accurate computations are however computer intensive and strategies should be established (sampling, averaging?) to limit the computation burden..The estimation of the net longwave radiation (NLW) at the surface is much further behind for two main reasons. First, it is more di

殺蟲(chóng)劑

right-atrium

echnic

The Solar Heat Input into the Upper Marine Environmentle optical input parameter in order to work. Three (four) such different input parameters have been selected for the reason that they are routinely measured on a global scale ensuring maximum solar heat input informations. The three versions of the model compare favorably with other more elaborate m