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Relationships between radiation, clouds, and convection during DYNAMO

Journal Article · · Journal of Geophysical Research: Atmospheres
DOI:https://doi.org/10.1002/2016JD025965· OSTI ID:1438683
 [1];  [1];  [2];  [3];  [3]
  1. Colorado State Univ., Fort Collins, CO (United States). Dept. of Atmospheric Science
  2. Univ. of California, Los Angeles, CA (United States). Joint Inst. for Regional Earth System Science and Engineering
  3. Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
In this paper, the relationships between radiation, clouds, and convection on an intraseasonal time scale are examined with data taken during the Dynamics of the Madden-Julian Oscillation (MJO) field campaign. Specifically, column-net, as well as vertical profiles of radiative heating rates, computed over Gan Island in the central Indian Ocean (IO) are used along with an objective analysis of large-scale fields to examine three MJO events that occurred during the 3 month period (October to December 2011) over this region. Longwave (LW) and shortwave radiative heating rates exhibit tilted structures, reflecting radiative effects associated with the prevalence of shallow cumulus during the dry, suppressed MJO phase followed by increasing deep convection leading into the active phase. As the convection builds going into the MJO active phase, there are increasingly top-heavy anomalous radiative heating rates while the column-net radiative cooling rate Qr progressively decreases. Temporal fluctuations in the cloud radiative forcing, being quite sensitive to changes in high cloudiness, are dominated by LW effects with an intraseasonal variation of ~0.4–0.6 K/d. While both the water vapor and cloud fields are inextricably linked, it appears that the tilted radiative structures are more related to water vapor effects. The intraseasonal variation of column-net radiative heating Qr enhances the convective signal in the mean by ~20% with a minimum in this enhancement ~10 days prior to peak MJO rainfall and maximum ~7 days after. Finally, this suggests that as MJO convective envelope weakens over the central IO, cloud-radiative feedbacks help maintain the mature MJO as it moves eastward.
Research Organization:
Colorado State Univ., Fort Collins, CO (United States); Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States); Univ. of California, Los Angeles, CA (United States)
Sponsoring Organization:
National Aeronautics and Space Administration (NASA) (United States); National Oceanic and Atmospheric Administration (NOAA) (United States); National Science Foundation (NSF) (United States); USDOE; USDOE Office of Science (SC), Biological and Environmental Research (BER) (SC-23)
Grant/Contract Number:
AC52-07NA27344; SC0008582
OSTI ID:
1438683
Alternate ID(s):
OSTI ID: 1377928
Report Number(s):
LLNL-JRNL--735094
Journal Information:
Journal of Geophysical Research: Atmospheres, Journal Name: Journal of Geophysical Research: Atmospheres Journal Issue: 5 Vol. 122; ISSN 2169-897X
Publisher:
American Geophysical UnionCopyright Statement
Country of Publication:
United States
Language:
English

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Shallow Circulations: Relevance and Strategies for Satellite Observation book January 2018
A Survey of Precipitation-Induced Atmospheric Cold Pools over Oceans and Their Interactions with the Larger-Scale Environment book January 2017
Shallow Circulations: Relevance and Strategies for Satellite Observation journal November 2017
A Survey of Precipitation-Induced Atmospheric Cold Pools over Oceans and Their Interactions with the Larger-Scale Environment journal November 2017
The Two Diurnal Modes of Tropical Upward Motion journal March 2019

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