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Double Tropopauses and the Tropical Belt Connected to ENSO
Hallgeir Wilhelmsen1,2,3, Florian Ladstädter1,3, Torsten Schmidt4
1Wegener Center for Climate and Global Change (WEGC) University of Graz Graz Austria.
This study reveals El Niño-Southern Oscillation (ENSO) influences double tropopause (DT) occurrences. More DTs appear during La Niña, while El Niño events reduce their frequency, impacting the tropopause region.
Area of Science:
- Atmospheric Science
- Climatology
- Geophysics
Background:
- Accurate, globally distributed data on the troposphere-stratosphere transition zone is crucial for analyzing double tropopause (DT) events.
- Radio occultation (RO) observations provide the necessary vertical resolution and accuracy for such analyses.
Purpose of the Study:
- To analyze the global and seasonal distribution of double tropopauses (DTs).
- To establish a connection between El Niño-Southern Oscillation (ENSO) phases and the occurrence and distribution of DTs.
Main Methods:
- Utilized radio occultation observations from 2001 to 2018.
- Analyzed global and seasonal characteristics of DTs in relation to ENSO phases.
Main Results:
- Identified hotspot locations for DTs, including near the subtropical jet stream and over high mountain ranges.
- Observed a higher frequency of DTs during the cold La Niña phase and lower rates during warmer El Niño events.
- Found that ENSO phases affect tropopause region structure, with La Niña correlating to lower first lapse rate tropopause altitude near the Niño 3 region.
Conclusions:
- ENSO significantly influences the occurrence and distribution of double tropopauses.
- La Niña conditions favor more DTs, while El Niño conditions lead to fewer, altering tropopause structure and the tropical belt width.
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