For reasons of computational economy the method is also appropriate for applications, in which hydrological and global circulation models (GCM) are coupled, and where computational effort becomes an issue.
In this work we present evidence that an abrupt shift, which encompassed marine circulation, hydrological and biological properties, occurred at the end of the 1980s in the Mediterranean Sea.
This study investigates the skill of linear methods for downscaling provincial-scale precipitation over Indonesia from fields that describe the large-scale circulation and hydrological cycle.
How might your research advance understanding of the challenges posed by climate change? A. Scientists have done a great job investigating and understanding how anthropogenic climate change will affect atmospheric circulation, the hydrological cycle, and weather extremes.
Accurately simulating precipitation processes and associated statistical rainfall properties (accumulation, instantaneous intensity and frequency of rainfall) with general circulation models is paramount for hydrological applications, numerical weather prediction and climate change studies.
An instrument called REMS is designed to provide new clues about the signature of the Martian general circulation, microscale weather systems, local hydrological cycle, destructive potential of UV radiation, and subsurface habitability based on ground-atmosphere interaction.
Calculations for the year 2050 are based on mean projected urban population, intensive livestock farming and discharge, derived from an ensemble of two IPCC emission scenarios (A2 - fast growth, and B1 - slow growth), three coupled atmosphere-ocean General Circulation Models (GCMs), and one Global Hydrological Model (GHM), i.e. WaterGAP36.
Analyses of changes in this aspect of variability under projected climate change scenarios are based on data from a multi-model ensemble of 19 General Circulation Models, which are used to drive hydrological models of the Okavango River and Delta.
A more intense hydrological cycle in a warmer world might make atmospheric circulation less energetic.
The possibility that a continuous or intermittent submarine source located at Volcano 1 or Volcano 8 (Fig. 2A) can indeed impact the surface ocean hydrological characteristics is considered by means of an ocean general circulation model (OGCM36).
