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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The Cloud Population and Onset of the Madden-Julian Oscillation over the Indian Ocean during dynamo-amieThe Cloud Population and Onset of the Madden-Julian Oscillation over the Indian Ocean during dynamo-amie
Department of Atmospheric Sciences, University of Washington, Seattle, Washington
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The Cloud Population and Onset of the Madden-Julian Oscillation over the Indian Ocean during dynamo-amieThe Cloud Population and Onset of the Madden-Julian Oscillation over the Indian Ocean during dynamo-amie
Department of Atmospheric Sciences, University of Washington, Seattle, Washington
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Professional: 2010- professor, Earth and Atmospheric Sciences, Georgia Institute of Technology 2002-2010 ProfessorProfessional: 2010- professor, Earth and Atmospheric Sciences, Georgia Institute of Technology 2002-2010 Professor
Consultant, Natural Resources Defense Council: “Predicting heat stress in Gujarat, India”
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Ocean Circulation Surface CurrentsOcean Circulation Surface Currents
About 10% of the ocean’s water is in surface currents, water flowing horizontally in the uppermost 400 m
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