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Increasing Water Vapor in the Stratosphere and Mesosphere After 2002
Author(s) -
Yue Jia,
Russell James,
Gan Quan,
Wang Tao,
Rong Pingping,
Garcia Rolando,
Mlynczak Martin
Publication year - 2019
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2019gl084973
Subject(s) - stratosphere , mesosphere , mesopause , microwave limb sounder , atmospheric sciences , water vapor , environmental science , atmosphere (unit) , depth sounding , climatology , aeronomy , latitude , meteorology , geology , physics , oceanography , geodesy
Water vapor (H 2 O) measurements made by the Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) instrument between 2002 and 2018 and by the Aura Microwave Limb Sounder (MLS) instrument between 2004 and 2018 are analyzed to determine the linear trend and solar cycle response of H 2 O in the stratosphere and mesosphere. Both SABER and MLS show a rapid global H 2 O increase of 5–6% per decade in the lower stratosphere after the 2001 drop. The increasing zonal mean H 2 O at 40°N in SABER and MLS is consistent with the Boulder frost point hygrometer data in the lower stratosphere. The global distribution of SABER and MLS H 2 O trends are positive at most altitudes and latitudes, and they peak in the tropical lower stratosphere. In the mesosphere the SABER H 2 O trend is 0.1–0.2 ppmv per decade and the MLS H 2 O trend is 0.2–0.3 ppmv per decade. The trend and solar cycle response derived from the observations are compared against the Whole Atmosphere Community Climate Model (WACCM). The solar cycle response of H 2 O from WACCM agrees with SABER and MLS. The linear H 2 O trend from WACCM does not show the observed increase in the lower stratosphere.