Identifying Signatures of Natural Climate Variability in Time Series of Global-Mean Surface Temperature: Methodology and Insights

Global-mean surface temperature is affected by both natural variability and anthropogenic forcing. This study is concerned with identifying and removing from global-mean temperatures the signatures of natural climate variability over the period January 1900–March 2009. A series of simple, physically...

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Bibliographic Details
Published in:	Journal of climate 2009-11, Vol.22 (22), p.6120-6141
Main Authors:	Thompson, David W. J., Wallace, John M., Jones, Phil D., Kennedy, John J.
Format:	Article
Language:	eng
Subjects:	20th century Advection Air masses Algorithms Anthropogenic factors Climate Climate change Climate variability Cold Colleges & universities Correlations Datasets Earth, ocean, space El Nino El Nino phenomena El Nino-Southern Oscillation event Estimates Exact sciences and technology External geophysics Global climate models Global warming Heat Human influences Instrumentation Land Land surface temperature Latitude Marine Mean temperatures Meteorology Natural variability Ocean temperature Oceans Sea level Sea surface Sea surface temperature Signatures Southern Oscillation Stratosphere Surface temperature Temperature Temperature effects Time series Variability Volcanic eruption effects Volcanic eruptions
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Summary:	Global-mean surface temperature is affected by both natural variability and anthropogenic forcing. This study is concerned with identifying and removing from global-mean temperatures the signatures of natural climate variability over the period January 1900–March 2009. A series of simple, physically based methodologies are developed and applied to isolate the climate impacts of three known sources of natural variability: the El Niño–Southern Oscillation (ENSO), variations in the advection of marine air masses over the highlatitude continents during winter, and aerosols injected into the stratosphere by explosive volcanic eruptions. After the effects of ENSO and high-latitude temperature advection are removed from the global-mean temperature record, the signatures of volcanic eruptions and changes in instrumentation become more clearly apparent. After the volcanic eruptions are subsequently filtered from the record, the residual time series reveals a nearly monotonic global warming pattern since ∼1950. The results also reveal coupling between the land and ocean areas on the interannual time scale that transcends the effects of ENSO and volcanic eruptions. Globally averaged land and ocean temperatures are most strongly correlated when ocean leads land by ∼2–3 months. These coupled fluctuations exhibit a complicated spatial signature with largest-amplitude sea surface temperature perturbations over the Atlantic Ocean.
ISSN:	0894-8755 1520-0442