Articles | Volume 21, issue 3
https://doi.org/10.5194/acp-21-2191-2021
https://doi.org/10.5194/acp-21-2191-2021
Research article
 | 
15 Feb 2021
Research article |  | 15 Feb 2021

Ice injected into the tropopause by deep convection – Part 2: Over the Maritime Continent

Iris-Amata Dion, Cyrille Dallet, Philippe Ricaud, Fabien Carminati, Thibaut Dauhut, and Peter Haynes

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Cited articles

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Dauhut, T., Chaboureau, J.-P., Mascart, P., and Lane, T.: The overshoots that hydrate the stratosphere in the tropics, EGU General Assembly, 4–13 April, 2018 in Vienna, Austria, EGU2018-9149, 2018. a
Short summary
Ice in the tropopause has a strong radiative effect on climate. The amount of ice injected (∆IWC) up to the tropical tropopause layer has been shown to be the highest over the Maritime Continent (MC), a region that includes Indonesia. ∆IWC is studied over islands and sea of the MC. Space-borne observations of ice, precipitation and lightning are used to estimate ∆IWC and are compared to ∆IWC estimated from the ERA5 reanalyses. It is shown that Java is the area of the greatest ∆IWC over the MC.
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