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

Viewed

Total article views: 2,513 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,936 514 63 2,513 61 63
  • HTML: 1,936
  • PDF: 514
  • XML: 63
  • Total: 2,513
  • BibTeX: 61
  • EndNote: 63
Views and downloads (calculated since 11 Oct 2019)
Cumulative views and downloads (calculated since 11 Oct 2019)

Viewed (geographical distribution)

Total article views: 2,513 (including HTML, PDF, and XML) Thereof 2,438 with geography defined and 75 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 23 Nov 2024
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.
Altmetrics
Final-revised paper
Preprint