Identification and separation of Mount Pinatubo and El Niño-Southern Oscillation land surface temperature anomalies

Fanglin Yang, Michael E. Schlesinger

Research output: Contribution to journalArticlepeer-review

Abstract

Empirical data analyses are performed to detect and separate the signals of the volcanic eruption and El Niño events in the observed surface air temperature (SAT) anomalies over land for the 2 years following the Pinatubo eruption. Composite analyses of surface temperatures for the 1950-1997 period, excluding the 2 years following each of the three major volcanic eruptions, Agung, El Chichón, and Pinatubo, show that the distribution of SAT anomalies over most land areas for the El Niño composite is opposite to that for the La Nina composite. The pattern of SAT anomalies changes from season to season. This feature is more prominent over North America than over the other continents. Singular value decomposition analyses show that following the Pinatubo eruption, El Niño signals were weak over Eurasia but relatively strong over the other continents. Over North America, the 1991-1992 El Niño event contributed more than 50% to the observed surface cooling of about -1.0°C in June, July, and August 1992. Globally averaged, the maximum cooling over land with the El Niño-Southern Oscillation signals removed is -0.5°C in September, October, and November 1992 and September, October, and November 1993.

Original languageEnglish (US)
Article number2001JD900146
Pages (from-to)14757-14770
Number of pages14
JournalJournal of Geophysical Research Atmospheres
Volume106
Issue numberD14
DOIs
StatePublished - Jul 27 2001

ASJC Scopus subject areas

  • Geophysics
  • Forestry
  • Oceanography
  • Aquatic Science
  • Ecology
  • Water Science and Technology
  • Soil Science
  • Geochemistry and Petrology
  • Earth-Surface Processes
  • Atmospheric Science
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science
  • Palaeontology

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