A comprehensive assessment of tropical stratospheric upwelling in the specified dynamics Community Earth System Model 1.2.2 – Whole Atmosphere Community Climate Model (CESM (WACCM))
Nicholas A. Davis,Sean M. Davis,Robert W. Portmann,Eric Ray,Karen H. Rosenlof,and Pengfei Yu
Cooperative Institute for Research in Environmental Sciences (CIRES), Chemical Sciences Division, NOAA Earth System Research Laboratory (ESRL), University of Colorado, Boulder, CO, USA
now at: Atmospheric Chemistry Observations and Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO, USA
Cooperative Institute for Research in Environmental Sciences (CIRES), Chemical Sciences Division, NOAA Earth System Research Laboratory (ESRL), University of Colorado, Boulder, CO, USA
Cooperative Institute for Research in Environmental Sciences (CIRES), Chemical Sciences Division, NOAA Earth System Research Laboratory (ESRL), University of Colorado, Boulder, CO, USA
now at: Institute for Environmental and Climate Research, Jinan University, Guangzhou, GD, China
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Total article views: 3,279 (including HTML, PDF, and XML)
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Large-scale waves drive upward motion in the tropical stratosphere, with major impacts on stratospheric chemistry and climate. However, some of the modeling methods which attempt to simulate the past evolution of the stratosphere do not seem to be able to recreate important trends. We believe this is due to disagreements between the basic climate of the model and observations, but if the method is constructed more carefully, the disagreement becomes smaller and the trends become more realistic.
Large-scale waves drive upward motion in the tropical stratosphere, with major impacts on...
