What Controls the Water Vapor Isotopic Composition Near the Surface of Tropical Oceans? Results From an Analytical Model Constrained by Large‐Eddy Simulations-Reference-Cited by-同舟云学术

What Controls the Water Vapor Isotopic Composition Near the Surface of Tropical Oceans? Results From an Analytical Model Constrained by Large‐Eddy Simulations

Published:2020-08 Issue:8 Volume:12 Page:
ISSN:1942-2466
Container-title:Journal of Advances in Modeling Earth Systems
language:en
Short-container-title:J. Adv. Model. Earth Syst.

Author:

Risi Camille¹^ORCID,Muller Caroline¹^ORCID,Blossey Peter²^ORCID

Affiliation:

1. Laboratoire de Meteorologie Dynamique, IPSL, CNRS, Ecole Normale Superieure Sorbonne Universite, PSL Research University Paris France

2. Department of Atmospheric Sciences University of Washington Seattle WA USA

Funder

H2020 European Research Council

National Aeronautics and Space Administration

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Environmental Chemistry,Global and Planetary Change

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020MS002106

Reference102 articles.

1. Isotope meteorology of cold front passages: A case study combining observations and modeling

2. Measuring variations of δ<sup>18</sup>O and δ<sup>2</sup>H in atmospheric water vapour using two commercial laser-based spectrometers: an instrument characterisation study

3. Detecting shifts in tropical moisture imbalances with satellite‐derived isotope ratios in water vapor

4. Importance of boundary layer mixing for the isotopic composition of surface vapor over the subtropical North Atlantic Ocean

5. Deuterium excess in marine water vapor: Dependency on relative humidity and surface wind speed during evaporation

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