Physical processes controlling the spatial distributions of relative humidity in the tropical tropopause layer over the Pacific-Reference-Cited by-同舟云学术

Physical processes controlling the spatial distributions of relative humidity in the tropical tropopause layer over the Pacific

Published:2017-06-13 Issue:11 Volume:122 Page:6094-6107
ISSN:2169-897X
Container-title:Journal of Geophysical Research: Atmospheres
language:en
Short-container-title:J. Geophys. Res. Atmos.

Author:

Jensen Eric J.¹,Thornberry Troy D.²³^ORCID,Rollins Andrew W.²³^ORCID,Ueyama Rei¹^ORCID,Pfister Leonhard¹^ORCID,Bui Theopaul¹^ORCID,Diskin Glenn S.⁴^ORCID,DiGangi Joshua P.⁴^ORCID,Hintsa Eric³⁵,Gao Ru‐Shan²^ORCID,Woods Sarah⁶^ORCID,Lawson R. Paul⁶^ORCID,Pittman Jasna⁷⁸

Affiliation:

1. Atmospheric Science BranchNASA Ames Research Center Moffett Field California USA

2. Chemical Sciences DivisionNOAA Earth System Research Laboratory Boulder Colorado USA

3. Cooperative Institute for Research in Environmental SciencesUniversity of Colorado Boulder Boulder Colorado USA

4. Chemistry and Dynamics BranchNASA Langley research Center Hampton Virginia USA

5. Global Monitoring DivisionNOAA Earth System Research Laboratory Boulder Colorado USA

6. SPEC, Inc. Boulder Colorado USA

7. Northwest Research Associates Seattle Washington USA

8. School of Engineering and Applied SciencesHarvard University Cambridge Massachusetts USA

Funder

NASA's Airborne Tropical Tropopause Experiment project

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017JD026632

Reference40 articles.

1. The quasi-biennial oscillation

2. Seasonal differences of vertical-transport efficiency in the tropical tropopause layer: On the interplay between tropical deep convection, large-scale vertical ascent, and horizontal circulations

3. Air parcel trajectory dispersion near the tropical tropopause

4. The AquaVIT-1 intercomparison of atmospheric water vapor measurement techniques

5. Tropical ozone as an indicator of deep convection

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