Positive low cloud and dust feedbacks amplify tropical North Atlantic Multidecadal Oscillation
Abstract
Abstract The Atlantic Multidecadal Oscillation (AMO) is characterized by a horseshoe pattern of sea surface temperature (SST) anomalies and has a wide range of climatic impacts. While the tropical arm of AMO is responsible for many of these impacts, it is either too weak or completely absent in many climate model simulations. Here we show, using both observational and model evidence, that the radiative effect of positive low cloud and dust feedbacks is strong enough to generate the tropical arm of AMO, with the low cloud feedback more dominant. The feedbacks can be understood in a consistent dynamical framework: weakened tropical trade wind speed in response to a warm middle latitude SST anomaly reduces dust loading and low cloud fraction over the tropical Atlantic, which warms the tropical North Atlantic SST. Together they contribute to the appearance of the tropical arm of AMO. Most current climate models miss both the critical wind speed response and two positive feedbacks though realistic simulations of them may be essential for many climatic studies related to the AMO.
- Authors:
-
- Joint Center for Earth Systems Technology University of Maryland, Baltimore County Catonsville Maryland USA, Earth Science Directorate NASA Goddard Space Flight Center Greenbelt Maryland USA
- Earth Science Directorate NASA Goddard Space Flight Center Greenbelt Maryland USA
- Program for Climate Modeling Diagnosis and Intercomparison Lawrence Livermore National Laboratory Livermore California USA
- Earth Science Directorate NASA Goddard Space Flight Center Greenbelt Maryland USA, Earth System Science Interdisciplinary Center University of Maryland College Park Maryland USA
- Scripps Institute of Oceanography University of California San Diego La Jolla California USA
- Earth Science Directorate NASA Goddard Space Flight Center Greenbelt Maryland USA, Goddard Earth Sciences Technology and Research Universities Space Research Association Columbia Maryland USA
- Publication Date:
- Research Org.:
- Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)
- Sponsoring Org.:
- USDOE Office of Science (SC)
- OSTI Identifier:
- 1249953
- Alternate Identifier(s):
- OSTI ID: 1261227; OSTI ID: 1409978
- Report Number(s):
- LLNL-JRNL-736933
Journal ID: ISSN 0094-8276
- Grant/Contract Number:
- AC52-07NA27344
- Resource Type:
- Published Article
- Journal Name:
- Geophysical Research Letters
- Additional Journal Information:
- Journal Name: Geophysical Research Letters Journal Volume: 43 Journal Issue: 3; Journal ID: ISSN 0094-8276
- Publisher:
- American Geophysical Union (AGU)
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES
Citation Formats
Yuan, Tianle, Oreopoulos, Lazaros, Zelinka, Mark, Yu, Hongbin, Norris, Joel R., Chin, Mian, Platnick, Steven, and Meyer, Kerry. Positive low cloud and dust feedbacks amplify tropical North Atlantic Multidecadal Oscillation. United States: N. p., 2016.
Web. doi:10.1002/2016GL067679.
Yuan, Tianle, Oreopoulos, Lazaros, Zelinka, Mark, Yu, Hongbin, Norris, Joel R., Chin, Mian, Platnick, Steven, & Meyer, Kerry. Positive low cloud and dust feedbacks amplify tropical North Atlantic Multidecadal Oscillation. United States. https://doi.org/10.1002/2016GL067679
Yuan, Tianle, Oreopoulos, Lazaros, Zelinka, Mark, Yu, Hongbin, Norris, Joel R., Chin, Mian, Platnick, Steven, and Meyer, Kerry. Thu .
"Positive low cloud and dust feedbacks amplify tropical North Atlantic Multidecadal Oscillation". United States. https://doi.org/10.1002/2016GL067679.
@article{osti_1249953,
title = {Positive low cloud and dust feedbacks amplify tropical North Atlantic Multidecadal Oscillation},
author = {Yuan, Tianle and Oreopoulos, Lazaros and Zelinka, Mark and Yu, Hongbin and Norris, Joel R. and Chin, Mian and Platnick, Steven and Meyer, Kerry},
abstractNote = {Abstract The Atlantic Multidecadal Oscillation (AMO) is characterized by a horseshoe pattern of sea surface temperature (SST) anomalies and has a wide range of climatic impacts. While the tropical arm of AMO is responsible for many of these impacts, it is either too weak or completely absent in many climate model simulations. Here we show, using both observational and model evidence, that the radiative effect of positive low cloud and dust feedbacks is strong enough to generate the tropical arm of AMO, with the low cloud feedback more dominant. The feedbacks can be understood in a consistent dynamical framework: weakened tropical trade wind speed in response to a warm middle latitude SST anomaly reduces dust loading and low cloud fraction over the tropical Atlantic, which warms the tropical North Atlantic SST. Together they contribute to the appearance of the tropical arm of AMO. Most current climate models miss both the critical wind speed response and two positive feedbacks though realistic simulations of them may be essential for many climatic studies related to the AMO.},
doi = {10.1002/2016GL067679},
journal = {Geophysical Research Letters},
number = 3,
volume = 43,
place = {United States},
year = {Thu Feb 04 00:00:00 EST 2016},
month = {Thu Feb 04 00:00:00 EST 2016}
}
https://doi.org/10.1002/2016GL067679
Web of Science
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