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Future changes in the relationship of precipitation intensity in Eastern Mediterranean with large scale circulation
Future changes relationship precipitation intensity Eastern Mediterranean large scale circulation
2010/9/13
The objective of this study is to investigate the linkage of large-scale upper air circulation over the greater European area with intense precipitation events over Eastern Mediterranean and then to e...
Simulated pre-industrial climate in Bergen Climate Model (version 2):model description and large-scale circulation features
Simulated pre-industrial climate Bergen Climate Model model description large-scale circulation features
2010/2/5
The Bergen Climate Model (BCM) is a fully-coupled atmosphere-ocean-sea-ice model that provides state-of-the-art computer simulations of the Earth's past, present, and future climate. Here, a pre-indus...
Determining the Mean, Large-Scale Circulation of the Atlantic with the Adjoint Method
Large-Scale Circulation Atlantic Adjoint Method
2008/12/19
A new model approach based on the adjoint formalism and aimed at assimilating large sets of hydrographic data is presented. The goal of the model calculations is to obtain the mean, large-scale ocean ...
Effects of Bottom Topography in the Large-Scale Circulation of the Southern Ocean
Bottom Topography Southern Ocean Large-Scale Circulation
2008/12/12
The characteristics of an unforced, stratified f-plane geostrophic flow over topography are described, and scaling arguments are made to justify the use of such a flow as a first-order approximation t...
Large-Scale Circulation with Locally Enhanced Vertical Mixing
Large-Scale Circulation intensified vertical mixing large-scale ocean model
2008/10/31
The influence of localized regions of intensified vertical mixing on the stratification and circulation in a large-scale ocean model is investigated with idealized numerical experiments. Numerical sol...
On the Ocean’s Large-Scale Circulation near the Limit of No Vertical Mixing
Large-Scale Circulation No Vertical Mixing Limit
2008/10/27
By convention, the ocean’s large-scale circulation is assumed to be a thermohaline overturning driven by the addition and extraction of buoyancy at the surface and vertical mixing in the interior. Pre...