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© Author(s) 2019. The contribution of deep convection to the amount of water vapour and ice in the tropical tropopause layer (TTL) from the tropical upper troposphere (UT; around 146 hPa) to the tropopause level (TL; around 100 hPa) is investigated.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::53d2f8a8f217df7a1934609575f8c696
Publikováno v:
Biblioteca Digital de Teses e Dissertações da PUC_RSPontifícia Universidade Católica do Rio Grande do SulPUC_RS.
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Introdu??o: A bronquiolite viral aguda (BVA) ? uma das princi
Introdu??o: A bronquiolite viral aguda (BVA) ? uma das princi
Externí odkaz:
http://tede2.pucrs.br/tede2/handle/tede/1369
The amount of ice injected into the tropical tropopause layer has a strong radiative impact on climate. A companion paper (Part 1) used the amplitude of the diurnal cycle of ice water content (IWC) as an estimate of ice injection by deep convection,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ed3671e7522931f282684f13adb0da8c