Quantification of dust-forced heating of the lower troposphere

P. Alpert*, Y. J. Kaufman, Y. Shay-El, D. Tanre, A. Da Silva, S. Schubert, J. H. Joseph

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

183 Scopus citations


Aerosols may affect climate through the absorption and scattering of solar radiation and, in the case of large dust particles, by interacting with thermal radiation. But whether atmospheric temperature responds significantly to such forcing has not been determined; feedback mechanisms could increase or decrease the effects of the aerosol forcing. Here we present an indirect measure of the tropospheric temperature response by explaining the 'errors' in the NASA/Goddard model/data-assimilation system. These errors, which provide information about physical processes missing from the predictive model, have monthly mean patterns that bear a striking similarity to observed patterns of dust over the eastern tropical North Atlantic Ocean. This similarity, together with the high correlations between latitudinal location of inferred maximum atmospheric heating rates and that of the number of dusty days, suggests that dust aerosols are an important source of inaccuracies in numerical weather-prediction models in this region. For the average dust event, dust is estimated to heat the lower atmosphere (1.5-3.5 km altitude) by ~0.2 K per day. At about 30 dusty days per year, the presence of the dust leads to a regional heating rate of ~6 K per year.

Original languageEnglish
Pages (from-to)367-370
Number of pages4
Issue number6700
StatePublished - 24 Sep 1998


Dive into the research topics of 'Quantification of dust-forced heating of the lower troposphere'. Together they form a unique fingerprint.

Cite this