Climate Dynamics

, Volume 43, Issue 5, pp 1439–1448

Uncertainty of AMSU-A derived temperature trends in relationship with clouds and precipitation over ocean

Authors

  • F. Weng
    • NOAA/NESDIS/Center for Satellite Applications and Research
    • Department of Earth, Ocean and Atmospheric ScienceFlorida State University
  • Z. Qin
    • NUIST/Center of Data Assimilation for Research and Application
Article

DOI: 10.1007/s00382-013-1958-7

Cite this article as:
Weng, F., Zou, X. & Qin, Z. Clim Dyn (2014) 43: 1439. doi:10.1007/s00382-013-1958-7

Abstract

Microwave Sounding Unit (MSU) and Advanced Microwave Sounding Unit-A (AMSU-A) observations from a series of National Oceanic and Atmospheric Administration satellites have been extensively utilized for estimating the atmospheric temperature trend. For a given atmospheric temperature condition, the emission and scattering of clouds and precipitation modulate MSU and AMSU-A brightness temperatures. In this study, the effects of the radiation from clouds and precipitation on AMSU-A derived atmospheric temperature trend are assessed using the information from AMSU-A window channels. It is shown that the global mean temperature in the low and middle troposphere has a larger warming rate (about 20–30 % higher) when the cloud-affected radiances are removed from AMSU-A data. It is also shown that the inclusion of cloud-affected radiances in the trend analysis can significantly offset the stratospheric cooling represented by AMSU-A channel 9 over the middle and high latitudes of Northern Hemisphere.

Keywords

Climate trend Satellite Cloud

Copyright information

© Springer-Verlag (outside the USA) 2013