The volcanic signal in surface temperature observations

349Citations
Citations of this article
92Readers
Mendeley users who have this article in their library.
Get full text

Abstract

Climate records of the past 140 yr are examined for the impact of major volcanic eruptions on surface temperature. After the low-frequency variations and El Nino/Southern Oscillation signal are removed, it is shown that for two years following great volcanic eruptions, the surface cools significantly by 0.1°-0.2°C in the global mean, in each hemisphere, and in the summer in the latitude bands 0° -30°S and 0° -30°N and by 0.3°C in the summer in the latitude band 30°-60°N. By contrast, in the first winter after major tropical eruptions and in the second winter after major high-latitude eruptions, North America and Eurasia warm by several degrees, while northern Africa and southwestern Asia cool by more than 0.5°C. -from Authors

Cite

CITATION STYLE

APA

Robock, A., & Jianping Mao. (1995). The volcanic signal in surface temperature observations. Journal of Climate, 8(5), 1086–1103. https://doi.org/10.1175/1520-0442(1995)008<1086:TVSIST>2.0.CO;2

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free