Opinion: Tropical cirrus – from micro-scale processes to climate-scale impacts

Autor(en)
Blaž Gasparini, Sylvia C. Sullivan, Adam B. Sokol, Bernd Kärcher, Eric Jensen, Dennis L. Hartmann
Abstrakt

Tropical cirrus clouds, i.e., any type of ice cloud with tops above 400hPa, play a critical role in the climate system and are a major source of uncertainty in our understanding of global warming. Tropical cirrus clouds involve processes spanning a wide range of spatial and temporal scales, from ice microphysics on cloud scales to mesoscale convective organization and planetary wave dynamics. This complexity makes tropical cirrus clouds notoriously difficult to model and has left many important questions stubbornly unanswered. At the same time, their multi-scale nature makes them well-positioned to benefit from the rise of global, high-resolution simulations of Earth's atmosphere and a growing abundance of remotely sensed and in situ observations. Rapid progress on our understanding of tropical cirrus requires coordinated efforts to take advantage of these modern computational and observational abilities. In this opinion paper, we review recent progress in cirrus studies, highlight important unanswered questions, and discuss promising paths forward. Significant progress has been made in understanding the life cycle of convectively generated "anvil"cirrus and the response of their macrophysical properties to large-scale controls. On the other hand, much work remains to be done to fully understand how small-scale anvil processes and the climatological anvil radiative effect will respond to global warming. Thin, in situ formed cirrus clouds are now known to be closely tied to the thermal structure and humidity of the tropical tropopause layer, but microphysical uncertainties prevent a full understanding of this link, as well as the precise amount of water vapor entering the stratosphere. Model representation of ice-nucleating particles, water vapor supersaturation, and ice depositional growth continue to pose great challenges to cirrus modeling. We believe that major advances in the understanding of tropical cirrus can be made through a combination of cross-tool synthesis and cross-scale studies conducted by cross-disciplinary research teams.

Organisation(en)
Institut für Meteorologie und Geophysik
Externe Organisation(en)
University of Arizona, University of Washington, Deutsches Zentrum für Luft- und Raumfahrt e.V. (DLR), NOAA Chemical Sciences Laboratory
Journal
Atmospheric Chemistry and Physics
Band
23
Seiten
15413-15444
Anzahl der Seiten
32
ISSN
1680-7316
DOI
https://doi.org/10.5194/acp-23-15413-2023
Publikationsdatum
12-2023
Peer-reviewed
Ja
ÖFOS 2012
105205 Klimawandel, 105206 Meteorologie
Schlagwörter
ASJC Scopus Sachgebiete
Atmospheric Science
Sustainable Development Goals
SDG 13 – Maßnahmen zum Klimaschutz
Link zum Portal
https://ucris.univie.ac.at/portal/de/publications/opinion-tropical-cirrus--from-microscale-processes-to-climatescale-impacts(a8d8d1e8-729c-4b0f-a860-bdf6992bf485).html