Air‐sea fluxes for Hurricane Patricia (2015): Comparison with supertyphoon Haiyan (2013) and under different ENSO conditions
Air‐sea fluxes for Hurricane Patricia (2015): Comparison with supertyphoon Haiyan (2013) and under different ENSO conditions
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DOI:
10.1002/2017jc012741
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发表时间:
2017-08
影响因子:
--
通讯作者:
Hsiao-Ching Huang;J. Boucharel;I. Lin;F. Jin;Chun-Chi Lien;I. Pun
中科院分区:
文献类型:
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作者:
Hsiao-Ching Huang;J. Boucharel;I. Lin;F. Jin;Chun-Chi Lien;I. Pun
Hurricane Patricia formed on October 20th, 2015 in the Eastern Pacific and, in less than 3 days, rapidly intensified from a Tropical Storm to a record-breaking hurricane with maximum sustained winds measured around 185 knots. It is almost 15 knots higher than 2013's supertyphoon Haiyan (the previous strongest tropical cyclone (TC) ever observed). This research focuses on analyzing the air-sea enthalpy flux conditions that contributed to hurricane Patricia's rapid intensification, and comparing them to supertyphoon Haiyan's. Despite a stronger cooling effect, a higher enthalpy flux supply is found during Patricia, in particular due to warmer pre-TC sea surface temperature conditions. This resulted in larger temperature and humidity differences at the air-sea interface, contributing to larger air-sea enthalpy heat fluxes available for Patricia's growth (24% more than for Haiyan). In addition, air-sea fluxes simulations were performed for hurricane Patricia under different climate conditions to assess specifically the impact of local and large-scale conditions on storm intensification associated with six different phases and types of El Nino Southern Oscillation (ENSO) and long-term climatological summer condition. We found that the Eastern Pacific El Nino developing and decaying summers, and the Central Pacific El Nino developing summer are the three most favorable ENSO conditions for storm intensification. This still represents a 37% smaller flux supply than in October 2015, suggesting that Patricia extraordinary growth is not achievable under any of these typical ENSO conditions but rather the result of the exceptional environmental conditions associated with the build-up of the strongest El Nino ever recorded.