نتایج جستجو برای: among nine general circulation models

تعداد نتایج: 2753132  

2007
A. M. de Boer D. M. Sigman J. R. Toggweiler J. L. Russell

[1] A growing number of paleoceanographic observations suggest that the ocean’s deep ventilation is stronger in warm climates than in cold climates. Here we use a general ocean circulation model to test the hypothesis that this relation is due to the reduced sensitivity of seawater density to temperature at low mean temperature; that is, at lower temperatures the surface cooling is not as effec...

2017
Hong Zhang S. A. Sannasiraj

Wind, wave and current interactions control the boundary fluxes, momentum and energy exchange between the atmosphere and the ocean, and within the water column. The wind wave effect on surface stress is investigated using a three-dimensional time-dependant ocean circulation model. The POM (Princeton Ocean Model) based model is implemented with realistic coastlines in South China Sea and emphasi...

2010
F. Richter D. Sidorenko S. Danilov J. Schröter

We analyse the North Atlantic circulation by combining data from ARGO profiling buoys and satellite altimetry measurements into an inverse finite-element ocean circulation model. The model solution is consistent with ocean dynamics and approximate conservation of temperature and salinity. The ocean circulation is analysed separately for the years 2005 and 2006. Temperature and salinity fields f...

تالی خشک, صادق, رستمی خلج, محمد, روحانی, حامد, سلمانی, حسین, محمدی, مجتبی,

  Concern about the impact of climate change on natural and socioeconomic systems has been increased in recent years and this issue caused an increasing interest in the scientific community . The aim of this study is to evaluate changes in parameters such as precipitation, minimum and maximum temperature by General Circulation Models (GCM) and its impact on average runoff using SWAT model in Gh...

Journal: :Tellus A: Dynamic Meteorology and Oceanography 1999

Journal: :Journal of the Meteorological Society of Japan. Ser. II 1983

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