Limitation of one-dimensional ocean models for coupled hurricane-ocean model forecasts
Wind stress imposed on the upper ocean by a hurricane can limit the hurricane's intensity primarily through shear-induced mixing of the upper ocean and subsequent cooling of the sea surface. Since shear-induced mixing is a one-dimensional process, some recent studies suggest that coupling a one...
| Published in: | Monthly Weather Review |
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| Main Authors: | , |
| Format: | Text |
| Language: | unknown |
| Published: |
DigitalCommons@URI
2009
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| Subjects: | |
| Online Access: | https://digitalcommons.uri.edu/gsofacpubs/1352 https://doi.org/10.1175/2009MWR2863.1 |
| Summary: | Wind stress imposed on the upper ocean by a hurricane can limit the hurricane's intensity primarily through shear-induced mixing of the upper ocean and subsequent cooling of the sea surface. Since shear-induced mixing is a one-dimensional process, some recent studies suggest that coupling a one-dimensional ocean model to a hurricane model may be sufficient for capturing the storm-induced sea surface temperature cooling in the region providing heat energy to the hurricane. Using both a one-dimensional and a three-dimensional version of the same ocean model, it is shown here that the neglect of upwelling, which can only be captured by a three-dimensional ocean model, underestimates the storm-core sea surface cooling for hurricanes translating at<~5ms-1. For hurricanes translating at <2ms-1, more than half of the storm-core sea surface cooling is neglected by the one-dimensional ocean model. Since the majority of hurricanes in the western tropical North Atlantic Ocean translate at<5ms-1, the idealized experiments presented here suggest that one-dimensional ocean models may be inadequate for coupled hurricane-ocean model forecasting. © 2009 American Meteorological Society. |
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