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Some of the material in is restricted to members of the community. By logging in, you may be able to gain additional access to certain collections or items. If you have questions about access or logging in, please use the form on the Contact Page.
Climate models currently struggle with the more traditional, coarse ( O(100 km) ) representation of the ocean. In these coarse ocean simulations, western boundary currents are notoriously difficult to model accurately. The modeled Gulf...
Northern high-latitude freshwater systems are an essential link between terrestrial and marine carbon cycles, transporting organic matter from ecosystems on land to the Arctic Ocean. However, polar regions are warming faster than the...
Initializing Coupled General Circulation Models (CGCMs) for routine seasonal ENSO prediction is currently an onerous task. This is one of the main reasons on why the CGCMs participating in the Coupled Model Intercomparison Project 5 ...
Using Lagrangian Model Simulations to Quantify the Sequestration Time of Remineralized CO2 in the California Current Ecosystem for Different Carbon Flux Pathways
The biological carbon pump encompasses three main pathways that transport particulate organic carbon from the surface ocean to depth; gravitational sinking, subduction, and active transport by vertically-migrating organisms. These three...
A hypothesis by Maul [1977], stating the rate of change of Loop Current (LC) volume is related to deep Yucatan Channel (YC) transport, is examined and validated with a continuous 54-year simulation of the regional 1/25˚ Gulf of Mexico ...
Coastal areas are very dynamic places, and a lot of that is due to the movement of waves and currents, which are responsible for disturbances on the seabed by causing shear-stress. Bed shear-stress can cause sediment motion and transport...
Some of the material in is restricted to members of the community. By logging in, you may be able to gain additional access to certain collections or items. If you have questions about access or logging in, please use the form on the Contact Page.
