Abstract
The upper-ocean thermodynamic observations forced by Hurricane Lili are analyzed. In the analysis of the overall energy budget, the density (mass) field is necessary for estimating the potential portion of mechanical energy. The density field is computed from the analyzed temperature and salinity observations. The interior part of the Loop Current warm core show little change after the storm's passage, while density increase (due to oceanic mixed layer cooling) is apparent in the Gulf of Mexico to the NW of the loop current.
| Original language | English (US) |
|---|---|
| Title of host publication | 26th Conference on Hurricanes and Tropical Meteorology |
| Pages | 619-620 |
| Number of pages | 2 |
| State | Published - 2004 |
| Externally published | Yes |
| Event | 26th Conference on Hurricanes and Tropical Meteorolgy - Miami, FL., United States Duration: May 3 2004 → May 7 2004 |
Other
| Other | 26th Conference on Hurricanes and Tropical Meteorolgy |
|---|---|
| Country | United States |
| City | Miami, FL. |
| Period | 5/3/04 → 5/7/04 |
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ASJC Scopus subject areas
- Engineering(all)
Cite this
Analyis of upper-ocean thermodynamic observations forced by Hurricane Lili. / Uhlhorn, Eric W.; Shay, Lynn K.
26th Conference on Hurricanes and Tropical Meteorology. 2004. p. 619-620.Research output: Chapter in Book/Report/Conference proceeding › Conference contribution
}
TY - GEN
T1 - Analyis of upper-ocean thermodynamic observations forced by Hurricane Lili
AU - Uhlhorn, Eric W.
AU - Shay, Lynn K
PY - 2004
Y1 - 2004
N2 - The upper-ocean thermodynamic observations forced by Hurricane Lili are analyzed. In the analysis of the overall energy budget, the density (mass) field is necessary for estimating the potential portion of mechanical energy. The density field is computed from the analyzed temperature and salinity observations. The interior part of the Loop Current warm core show little change after the storm's passage, while density increase (due to oceanic mixed layer cooling) is apparent in the Gulf of Mexico to the NW of the loop current.
AB - The upper-ocean thermodynamic observations forced by Hurricane Lili are analyzed. In the analysis of the overall energy budget, the density (mass) field is necessary for estimating the potential portion of mechanical energy. The density field is computed from the analyzed temperature and salinity observations. The interior part of the Loop Current warm core show little change after the storm's passage, while density increase (due to oceanic mixed layer cooling) is apparent in the Gulf of Mexico to the NW of the loop current.
UR - http://www.scopus.com/inward/record.url?scp=3042742756&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=3042742756&partnerID=8YFLogxK
M3 - Conference contribution
SP - 619
EP - 620
BT - 26th Conference on Hurricanes and Tropical Meteorology
ER -