skip to main content

DOE PAGESDOE PAGES

Title: Cloud and circulation feedbacks in a near-global aquaplanet cloud-resolving model

A near-global aquaplanet cloud-resolving model (NGAqua) with fixed meridionally varying sea-surface temperature (SST) is used to investigate cloud feedbacks due to three climate perturbations: a uniform 4 K SST increase, a quadrupled-CO2 concentration, and both combined. NGAqua has a horizontal resolution of 4 km with no cumulus parameterization. Its domain is a zonally periodic 20,480 km-long tropical channel, spanning 46°S–N. It produces plausible mean distributions of clouds, rainfall, and winds. After spin-up, 80 days are analyzed for the control and increased-SST simulations, and 40 days for those with quadrupled CO 2. The Intertropical Convergence Zone width and tropical cloud cover are not strongly affected by SST warming or CO 2 increase, except for the expected upward shift in high clouds with warming, but both perturbations weaken the Hadley circulation. Increased SST induces a statistically significant increase in subtropical low cloud fraction and in-cloud liquid water content but decreases midlatitude cloud, yielding slightly positive domain-mean shortwave cloud feedbacks. CO 2 quadrupling causes a slight shallowing and a statistically insignificant reduction of subtropical low cloud fraction. Warming-induced low cloud changes are strongly correlated with changes in estimated inversion strength, which increases modestly in the subtropics but decreases in the midlatitudes. Enhanced clear-skymore » boundary layer radiative cooling in the warmer climate accompanies the robust subtropical low cloud increase. The probability distribution of column relative humidity across the tropics and subtropics is compared between the control and increased-SST simulations. It shows no evidence of bimodality or increased convective aggregation in a warmer climate.« less
Authors:
ORCiD logo [1] ; ORCiD logo [1] ;  [2]
  1. Univ. of Washington, Seattle, WA (United States). Dept. of Atmospheric Sciences
  2. Stony Brook Univ. of New York, NY (United States). School of Marine and Atmospheric Sciences
Publication Date:
Grant/Contract Number:
SC0012451; SC0012488
Type:
Published Article
Journal Name:
Journal of Advances in Modeling Earth Systems
Additional Journal Information:
Journal Volume: 9; Journal Issue: 2; Journal ID: ISSN 1942-2466
Publisher:
American Geophysical Union (AGU)
Research Org:
Univ. of Washington, Seattle, WA (United States); Stony Brook Univ. of New York, NY (United States)
Sponsoring Org:
USDOE Office of Science (SC)
Country of Publication:
United States
Language:
English
Subject:
58 GEOSCIENCES
OSTI Identifier:
1355939
Alternate Identifier(s):
OSTI ID: 1355940; OSTI ID: 1393561

Narenpitak, Pornampai, Bretherton, Christopher S., and Khairoutdinov, Marat F.. Cloud and circulation feedbacks in a near-global aquaplanet cloud-resolving model. United States: N. p., Web. doi:10.1002/2016MS000872.
Narenpitak, Pornampai, Bretherton, Christopher S., & Khairoutdinov, Marat F.. Cloud and circulation feedbacks in a near-global aquaplanet cloud-resolving model. United States. doi:10.1002/2016MS000872.
Narenpitak, Pornampai, Bretherton, Christopher S., and Khairoutdinov, Marat F.. 2017. "Cloud and circulation feedbacks in a near-global aquaplanet cloud-resolving model". United States. doi:10.1002/2016MS000872.
@article{osti_1355939,
title = {Cloud and circulation feedbacks in a near-global aquaplanet cloud-resolving model},
author = {Narenpitak, Pornampai and Bretherton, Christopher S. and Khairoutdinov, Marat F.},
abstractNote = {A near-global aquaplanet cloud-resolving model (NGAqua) with fixed meridionally varying sea-surface temperature (SST) is used to investigate cloud feedbacks due to three climate perturbations: a uniform 4 K SST increase, a quadrupled-CO2 concentration, and both combined. NGAqua has a horizontal resolution of 4 km with no cumulus parameterization. Its domain is a zonally periodic 20,480 km-long tropical channel, spanning 46°S–N. It produces plausible mean distributions of clouds, rainfall, and winds. After spin-up, 80 days are analyzed for the control and increased-SST simulations, and 40 days for those with quadrupled CO2. The Intertropical Convergence Zone width and tropical cloud cover are not strongly affected by SST warming or CO2 increase, except for the expected upward shift in high clouds with warming, but both perturbations weaken the Hadley circulation. Increased SST induces a statistically significant increase in subtropical low cloud fraction and in-cloud liquid water content but decreases midlatitude cloud, yielding slightly positive domain-mean shortwave cloud feedbacks. CO2 quadrupling causes a slight shallowing and a statistically insignificant reduction of subtropical low cloud fraction. Warming-induced low cloud changes are strongly correlated with changes in estimated inversion strength, which increases modestly in the subtropics but decreases in the midlatitudes. Enhanced clear-sky boundary layer radiative cooling in the warmer climate accompanies the robust subtropical low cloud increase. The probability distribution of column relative humidity across the tropics and subtropics is compared between the control and increased-SST simulations. It shows no evidence of bimodality or increased convective aggregation in a warmer climate.},
doi = {10.1002/2016MS000872},
journal = {Journal of Advances in Modeling Earth Systems},
number = 2,
volume = 9,
place = {United States},
year = {2017},
month = {5}
}