Tropical convective outflow and near surface equivalent potential temperatures

Ian Folkins, Samuel J. Oltmans, Anne M. Thompson

Research output: Contribution to journalArticlepeer-review

41 Scopus citations

Abstract

We use clear sky heating rates to show that convective outflow in the tropics decreases rapidly with height between the 350 K and 360 K potential temperature surfaces (or between roughly 13 and 15 km). There is also a rapid fall-off in the pseudoequivalent potential temperature probability distribution of near surface air parcels between 350 K and 360 K. This suggests that the vertical variation of convective outflow in the upper tropical troposphere is to a large degree determined by the distribution of sub cloud layer entropy.

Original languageEnglish (US)
Pages (from-to)2549-2552
Number of pages4
JournalGeophysical Research Letters
Volume27
Issue number16
DOIs
StatePublished - Aug 15 2000

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Earth and Planetary Sciences(all)

Fingerprint Dive into the research topics of 'Tropical convective outflow and near surface equivalent potential temperatures'. Together they form a unique fingerprint.

Cite this