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Title: The strength of the tropical inversion and its response to climate change in 18 CMIP5 models

Journal Article · · Climate Dynamics
 [1];  [1];  [2];  [2]
  1. Univ. of California, Los Angeles, CA (United States)
  2. Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)

In this work, we examine the tropical inversion strength, measured by the estimated inversion strength (EIS), and its response to climate change in 18 models associated with phase 5 of the coupled model intercomparison project (CMIP5). While CMIP5 models generally capture the geographic distribution of observed EIS, they systematically underestimate it off the west coasts of continents, due to a warm bias in sea surface temperature. The negative EIS bias may contribute to the low bias in tropical low-cloud cover in the same models. Idealized perturbation experiments reveal that anthropogenic forcing leads directly to EIS increases, independent of “temperature-mediated” EIS increases associated with long-term oceanic warming. This fast EIS response to anthropogenic forcing is strongly impacted by nearly instantaneous continental warming. The temperature-mediated EIS change has contributions from both uniform and non-uniform oceanic warming. The substantial EIS increases in uniform oceanic warming simulations are due to warming with height exceeding the moist adiabatic lapse rate in tropical warm pools. EIS also increases in fully-coupled ocean–atmosphere simulations where CO2 concentration is instantaneously quadrupled, due to both fast and temperature-mediated changes. The temperature-mediated EIS change varies with tropical warming in a nonlinear fashion: The EIS change per degree tropical warming is much larger in the early stage of the simulations than in the late stage, due to delayed warming in the eastern parts of the subtropical oceans. Given the importance of EIS in regulating tropical low-cloud cover, this suggests that the tropical low-cloud feedback may also be nonlinear.

Research Organization:
Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)
Sponsoring Organization:
USDOE National Nuclear Security Administration (NNSA)
Grant/Contract Number:
AC52-07NA27344
OSTI ID:
1772308
Report Number(s):
LLNL-JRNL-652004; 772398
Journal Information:
Climate Dynamics, Vol. 45, Issue 1-2; ISSN 0930-7575
Publisher:
Springer-VerlagCopyright Statement
Country of Publication:
United States
Language:
English

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Cited By (15)

Feedback mechanisms of shallow convective clouds in a warmer climate as demonstrated by changes in buoyancy journal May 2018
Processes Responsible for Cloud Feedback journal October 2016
Relationships Between Inversion Strength, Lower-Tropospheric Moistening, and Low-Cloud Fraction in the Subtropical Southeast Pacific Derived From Stable Isotopologues of Water Vapor journal August 2018
Insights into low-latitude cloud feedbacks from high-resolution models journal November 2015
Low-Cloud Feedbacks from Cloud-Controlling Factors: A Review journal October 2017
The Cloud Feedback Model Intercomparison Project (CFMIP) contribution to CMIP6 journal January 2017
A refined model for the Earth’s global energy balance journal May 2019
Mechanisms Behind the Extratropical Stratiform Low‐Cloud Optical Depth Response to Temperature in ARM Site Observations journal February 2019
Cloud feedback mechanisms and their representation in global climate models: Cloud feedback mechanisms and their representation in GCMs journal May 2017
Temporal and spatial variability of elevated inversions over Europe based on ERA‐Interim reanalysis journal August 2019
Seasonally variant low cloud adjustment over cool oceans journal October 2018
Relationship of tropospheric stability to climate sensitivity and Earth’s observed radiation budget journal November 2017
The summer diurnal cycle of coastal cloudiness over west Iberia using Meteosat/SEVIRI and a WRF regional climate model simulation: DIURNAL CYCLE OF SUMMER CLOUDINESS OVER WEST IBERIA journal August 2015
Low-Cloud Feedbacks from Cloud-Controlling Factors: A Review book May 2016
Impact of decadal cloud variations on the Earth’s energy budget journal October 2016

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