3 Current Capabilities and Limitations3 Current Capabilities and Limitations
Doppler radars, usage and quality of satellite data, improvements in nwp model physics, and the use of these observations through more sophisticated data assimilation capabilities to provide improved initial conditions for the models
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Observed subseasonal variability of oceanic barrier and compensated layersObserved subseasonal variability of oceanic barrier and compensated layers
There is significant variability of anomalous barrier layer and compensated layer width on interannual periods, while in the North Pacific longer term changes are also detectable
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Prediction from Weeks to DecadesPrediction from Weeks to Decades
Ben Kirtman, David Anderson, Gilbert Brunet, In-Sik Kang, Adam Scaife and Doug Smith
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The ocean observing system for tropical cyclone intensification forecasts and studiesThe ocean observing system for tropical cyclone intensification forecasts and studies
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On the development of a Regional Hydrodynamic Model around Florida Bay and the Florida KeysOn the development of a Regional Hydrodynamic Model around Florida Bay and the Florida Keys
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Ocean Salinity & Density Currents Class Copy Ocean Salinity Oceans are saltyOcean Salinity & Density Currents Class Copy Ocean Salinity Oceans are salty
Salts make up 99. 7% of the ocean’s dissolved materials. The common term to describe the dissolved salts in seawater is salinity. Ocean water contains many different kinds of salts, but the most abundant is sodium chloride (NaCl)
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Tropical Atlantic Biases in ccsm4Tropical Atlantic Biases in ccsm4
Abf a similar problem arises in the coupled model if the atmospheric component produces alongshore winds that are too weak. Erroneously warm coastal ssts spread westward through a combination of advection and positive air-sea feedback involving marine
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Prediction from Weeks to DecadesPrediction from Weeks to Decades
Decadal Variability (amv); trend among others. Some of the outstanding challenges include how to evaluate and validate prediction systems, how to improve models and prediction systems
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Variability of the Oceanic Mixed Layer 1960-2004Variability of the Oceanic Mixed Layer 1960-2004
Sst, suggesting that other processes such as advection are more important. Interestingly, at decadal periods the winter-spring mixed layers of both basins show trends, deepening by 10-40m over the 45-year period of this analysis
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