Articles | Volume 18, issue 7
https://doi.org/10.5194/acp-18-4597-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-18-4597-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Nonlinear response of tropical lower-stratospheric temperature and water vapor to ENSO
Chaim I. Garfinkel
CORRESPONDING AUTHOR
The Fredy and Nadine Herrmann Institute of Earth Sciences, Hebrew University of Jerusalem, Jerusalem, Israel
Amit Gordon
The Fredy and Nadine Herrmann Institute of Earth Sciences, Hebrew University of Jerusalem, Jerusalem, Israel
Luke D. Oman
NASA Goddard Space Flight Center, Greenbelt, MD, USA
Feng Li
Universities Space Research Association, Columbia, MD, USA
Sean Davis
NOAA Earth System Research Laboratory, Boulder, CO, USA
Steven Pawson
NASA Goddard Space Flight Center, Greenbelt, MD, USA
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Latest update: 14 Dec 2024
Short summary
The impact of El Niño in the lower stratosphere is nonlinear in spring. While moderate El Niño events lead to cooling in this region,
strong El Niño events appear to lead to warming, and hence the water vapor response is nonlinear too. The net effect is that strong
El Nino events, such as in 1997/1998 and 2015/2016, lead to qualitatively different water vapor impacts as compared to moderate
El Nino events.
The impact of El Niño in the lower stratosphere is nonlinear in spring. While moderate El Niño...
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