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Trends in Global Temperature: Appendix

Overview

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In this appendix to Trends in Global Temperature, we examine monthly anomalies, seasonal anomalies, and mean global temperature in degrees centigrade. The Northern Hemisphere has generally warmed more than the Southern. This gap emerged in about 1920, disappeared between 1965 and 1990, but has re-emerged. Warming in the Northern Hemisphere has been most severe in the Arctic. Between 1920 and 1960, the Arctic was warmer than normal, and the Antarctic was colder than normal.  Since 1980, both Arctic and Antarctic have been warmer than normal, with the greatest warming occurring in the Arctic.

Monthly Analysis of Global Temperature Anomalies, 1880-2007

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In the analysis below, we examine monthly changes in anomalies.

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Seasonal Temperature Anomalies

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We grouped anomalies into the four seasons, to see whether the warming has been uniform.  We find that spring has warmed the most (-1312.43 + 0.675367 x), followed by winter (-1266.02 + 0.65162 x), then summer (-1182.94 + 0.609115 x) then fall (-1044.01 + 0.5385 x).

Mean Global Temperature, Degrees Centigrade

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In the analysis below, we have used NASA's GISS Surface Temperature Analysis, and converted their anomaly data to degrees centigrade. The GISS analysis of global surface temperature, documented in the scientific literature, incorporates data from three data bases made available monthly: (1) the Global Historical Climatology Network (GHCN) of the National Climate Data Center, (2) the satellite analysis of global sea surface temperature of Reynolds et al., and (3) Antarctic records of the Scientific Committee on Antarctic Research (SCAR)

Sources : GHCN 1880 - 11/2008 meteorological stations, using elimination of outliers and homogeneity adjustment.Downloaded from http://data.giss.nasa.gov/gistemp/tabledata/GLB.Ts.txt.

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Variations by Latitude

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NASA reports annual mean land-ocean temperature index in .01 C anomalies for selected zones. Their sources include GHCN (Novwember, 1880-2008), HadISST1 (November, 1880-1981), and Reynolds v2 (December 1981-November 2008). They used an anomaly base period of 1951-1980, eliminated outliers, and did a homogeneity adjustment.

The first graph below shows that the Northern Hemisphere has generally warmed more than the Southern. This gap emerged in about 1920, disappeared between 1965 and 1990, but has re-emerged.

The second graph below shows the warming in the Northern Hemisphere has been most severe in the arctic. The four lines depict anomalies from the equator to 24 degrees N., 24-44 N., 44-64 N, and 64-90 degrees N.

A third graph compares the Arctic and Antarctic anomalies.  Between 1920 and 1960, the Arctic was warmer than normal, and the Antarctic was colder than normal.  Since 1980, both Arctic and Antarctic have been warmer than normal, with the greatest warming occurring in the Arctic.

Source: http://data.giss.nasa.gov/gistemp/tabledata/ZonAnn.Ts+dSST. txt

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References

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Hansen, J., R. Ruedy, J. Glascoe, and Mki. Sato, 1999: GISS analysis of surface temperature change. J. Geophys. Res., 104, 30997-31022, doi:10.1029/1999JD900835. http://pubs.giss.nasa.gov/abstracts/1999/Hansen_etal.html

Peterson, T.C., and R.S. Vose, 1997: An overview of the Global Historical Climatology Network temperature database. Bull. Amer. Meteorol. Soc. 78, 2837-2849.

Reynolds, R.W., and T.M. Smith, 1994: Improved global sea surface temperature analyses. J. Climate 7, 929-948.

Scientific Committee on Antarctic Research (SCAR), www.scar.org.

Other Papers in this Series

© 2009 David Stang. All rights reserved.

Dr. Stang is available for presentations on this topic. Contact him by email.

Last Revised: Sunday, January 11, 2009