Publication Date:
2018-06-08
Description:
The new MLS data are consistent with convective input of H(sub 2)O into the bottom of the TTL followed by slow ascent with a maximum relative amplitude in the seasonal cycle occurring near the tropopause nearly in phase with the tropopause temperature seasonal cycle.
Keywords:
Geophysics
Type:
Journal of Geophysical Research; Volume 109; d06110-d01029
Format:
text