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• W1567882839 abstract "[1] Deep convection associated with tropical cyclones (TCs) is considered to play an important role in the tropical troposphere-to-stratosphere transport (TST). In this study, both the AIRS satellite measurements on Aqua and the Interim reanalysis of the European Centre for Medium-Range Weather Forecasts (ERA-Interim) are used to estimate the contribution of TCs to the tropical TST over the western North Pacific (WNP). A case study for Typhoon Nock-ten (2004) demonstrates that both the AIRS and the ERA-Interim data can infer the direct transport of the tropospheric air into the lower stratosphere in the vicinity of the TC eyewall. A contrast analysis for the inactive and active TC seasons of 2003 and 2004 over the WNP based on the same data sets suggests that in the region where TCs occur frequently the TST is significantly enhanced. As a result, the TC-induced TST in the active TC season is about 25% higher than that in the inactive TC season. The results based on the ERA-Interim data for the TC seasons over the WNP from 1989 to 2010 show that TCs can account for more than 10% of the total TST in most of the impact region with the highest contribution up to 30%. Over the entire WNP, TCs account for about 5.6% of the total TST and about 10.9% of the total upward transport across the base of the Tropical Transition Layer (TTL). This suggests that TCs could have a significant contribution to the total upward transport into the TTL over the WNP." @default.
• W1567882839 created "2016-06-24" @default.
• W1567882839 creator A5013559365 @default.
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• W1567882839 date "2012-06-27" @default.
• W1567882839 modified "2023-10-03" @default.
• W1567882839 title "Contribution of tropical cyclones to stratosphere-troposphere exchange over the northwest Pacific: Estimation based on AIRS satellite retrievals and ERA-Interim data" @default.
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• W1567882839 doi "https://doi.org/10.1029/2012jd017494" @default.
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