Abstract
Mesoscale convective systems (MCSs) play a dominant role in tropical climate. However, the variabilities of their occurrences on a tropical-wide scale remain elusive, and the way they impact the tropical stratospheric moisture remains under debate. Based on a comprehensive global MCS data set during 1985–2008, we detect distinct transitions in tropical MCS activities, with the occurrence frequency of MCS during 1995–2002 being significantly lower than those before and after this period by over 10%. The stepwise transition of tropical MCSs has a significant impact on stratospheric water vapor: Active MCS occurrences result in an overall drier stratosphere, and vice versa. We demonstrate that these changes are closely related to the sea surface temperature pattern in the tropical central Pacific and the associated Walker circulation shift on convective systems. Our results suggest that the sea surface temperature variability in tropical central Pacific may exert an important forcing on the stratospheric water vapor.
| Original language | English |
|---|---|
| Article number | e2019GL086320 |
| Journal | Geophysical Research Letters |
| Volume | 47 |
| Issue number | 5 |
| DOIs | |
| State | Published - Mar 16 2020 |
Keywords
- Walker circulation
- equatorial central Pacific
- mesoscale convective system
- sea surface temperature
- stratospheric water vapor
- tropical climate