Titlebook: Large-Scale Transport Processes in Oceans and Atmosphere; J. Willebrand,D. L. T. Anderson Book 1986 Springer Science+Business Media Dordre

MOURN

書目名稱Large-Scale Transport Processes in Oceans and Atmosphere影響因子(影響力)




書目名稱Large-Scale Transport Processes in Oceans and Atmosphere影響因子(影響力)學(xué)科排名




書目名稱Large-Scale Transport Processes in Oceans and Atmosphere網(wǎng)絡(luò)公開度




書目名稱Large-Scale Transport Processes in Oceans and Atmosphere網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Large-Scale Transport Processes in Oceans and Atmosphere被引頻次




書目名稱Large-Scale Transport Processes in Oceans and Atmosphere被引頻次學(xué)科排名




書目名稱Large-Scale Transport Processes in Oceans and Atmosphere年度引用




書目名稱Large-Scale Transport Processes in Oceans and Atmosphere年度引用學(xué)科排名




書目名稱Large-Scale Transport Processes in Oceans and Atmosphere讀者反饋




書目名稱Large-Scale Transport Processes in Oceans and Atmosphere讀者反饋學(xué)科排名

Delirium

Diagnostic Models of Ocean Circulation,ctives of the diagnostic approach include the determination of circulation parameters (in particular the three-dimensional velocity field) and the testing of dynamical concepts (especially the role of mixing in the budgets of heat, salt and potential vorticity).

培養(yǎng)

1389-2185 es of WCRP are to determine the extent to which climate change can be predicted, and the extent to which human activities (such as increasing the level of CO ) can influence our climate. 2 To understand and possibly to predict climate change, one needs a good understanding of the dynamics of the oce

同時發(fā)生

Maximum Entropy Production as a Constraint in Climate Models,rch for simple “l(fā)aws” which control the mean system. (Here a mean would usually be a time average over years or longer with, in addition, possible spatial averaging.) Progress towards a solution to the climate problem is likely to come about by a combination of these two methods.

Constituent

彎曲的人

提名

Thermohaline Effects in the Ocean Circulation and Related Simple Models,” developed the instruments needed to measure these and other oceanographic parameters of interest with the required accuracy. They also developed the theoretical tools by help of which the ocean currents could be calculated from the measured temperature and salinity fields, in particular the so-called “dynamic method”.

voluble

沖突

Some Topics in the General Circulation of the Atmosphere,of equations are used to investigate the importance of orographic and thermal forcing and the role played by transients on the synoptic and longer time-scales..The usefulness of considering maps of potential vorticity on isentropic surfaces for the diagnosis of the behaviour of synoptic systems in t

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