Global Surface Temperature Anomalies
Background Information - FAQ
What is a temperature anomaly?
The term temperature anomaly means a departure from a reference value or long-term average. A positive anomaly indicates that the observed temperature was warmer than the reference value, while a negative anomaly indicates that the observed temperature was cooler than the reference value.
What can the mean global temperature anomaly be used for?
This product is a global-scale climate diagnostic tool and provides a big picture overview of average global temperatures compared to a reference value.
What datasets are used in calculating the average global temperature anomaly?
Land surface temperatures are available from the Global Historical Climate Network-Monthly (GHCN-M). Sea surface temperatures are determined using the extended reconstructed sea surface temperature (ERSST) analysis. ERSST uses the most recently available International Comprehensive Ocean-Atmosphere Data Set (ICOADS) and statistical methods that allow stable reconstruction using sparse data. The monthly analysis begins January 1854, but due to very sparse data, no global averages are computed before 1880. With more observations after 1880, the signal is stronger and more consistent over time.
What version of the GHCN-M analysis is currently being used?
Effective September 2012, the GHCN-M version 3.2.0 dataset of monthly mean temperature replaced the GHCN-M version 3.1.0 monthly mean temperature dataset. Beginning with the August 2012 Global monthly State of the Climate Report, released on September 17, 2012, GHCN-M version 3.2.0 is used for NCDC climate monitoring activities, including calculation of global land surface temperature anomalies and trends. For more information about this newest version, please see the GHCN-M version 3.2.0 Technical Report.
*The GHCN-M version 3.1.0 Technical Report was revised on September 5, 2012 to accurately reflect the changes incorporated in that version. Previously that report incorrectly included discussion of changes to the Pairwise Homogeneity Algorithm (PHA). Changes to the PHA are included in version 3.2.0 and described in the version 3.2.0 Technical Report. Please see the Frequently Asked Questions to learn more about this update.
What version of the ERSST analysis is currently being used?
ERSST version 3b is currently used. ERSST version 3 improved upon version 2 in several ways: first, by changing the low-frequency tuning, effectively increasing the sensitivity to data prior to 1930; by internally handling sea ice calculations to increase the timeliness of the dataset; and by using satellite observations to increase data where in-situ measurements are sparse (Smith et al., 2008). In version 3b, the satellite observations were removed from the product because they were found to have introduced a bias that caused problems for many of our users. The bias was strongest in the middle and high latitude Southern Hemisphere where in-situ (ship and buoy) observations are sparse. More detailed information about the switch to version 3b.
When was the use of the ERSST version 3b implemented?
The transition to the new ERSST version (3b) occurred in November 2008. The Climate Monitoring Branch began using the updated merged land-ocean dataset for the July 2009 State of the Climate Report. The changes were previewed in the May and June 2009 State of the Climate reports to caution users.
Why use temperature anomalies (departure from average) and not absolute temperature measurements?
Absolute estimates of global average surface temperature are difficult to compile for several reasons. Some regions have few temperature measurement stations (e.g., the Sahara Desert) and interpolation must be made over large, data-sparse regions. In mountainous areas, most observations come from the inhabited valleys, so the effect of elevation on a region's average temperature must be considered as well. For example, a summer month over an area may be cooler than average, both at a mountain top and in a nearby valley, but the absolute temperatures will be quite different at the two locations. The use of anomalies in this case will show that temperatures for both locations were below average.
Using reference values computed on smaller [more local] scales over the same time period establishes a baseline from which anomalies are calculated. This effectively normalizes the data so they can be compared and combined to more accurately represent temperature patterns with respect to what is normal for different places within a region.
For these reasons, large-area summaries incorporate anomalies, not the temperature itself. Anomalies more accurately describe climate variability over larger areas than absolute temperatures do, and they give a frame of reference that allows more meaningful comparisons between locations and more accurate calculations of temperature trends.
How is the average global temperature anomaly time-series calculated?
The global time series is produced from the Smith and Reynolds blended land and ocean data set (Smith et al., 2008). This data set consists of monthly average temperature anomalies on a 5° x 5° grid across land and ocean surfaces. These grid boxes are then averaged to provide an average global temperature anomaly. An area-weighted scheme is used to reflect the reality that the boxes are smaller near the poles and larger near the equator. Global-average anomalies are calculated on a monthly and annual time scale. Average temperature anomalies are also available for land and ocean surfaces separately, and the Northern and Southern Hemispheres separately. The global and hemispheric anomalies are provided with respect to the period 1901-2000, the 20th century average.
Why do some of the products use different reference periods?
The maps show temperature anomalies relative to the 1981–2010 base period. This period is used in order to comply with a recommended World Meteorological Organization (WMO) Policy, which suggests using the latest decade for the 30-year average. For the global-scale averages (global land and ocean, land-only, ocean-only, and hemispheric time series), the reference period is adjusted to the 20th Century average for conceptual simplicity (the period is more familiar to more people, and establishes a longer-term average). The adjustment does not change the shape of the time series or affect the trends within it.
How often and when is the global average temperature dataset updated?
The dataset is updated every month. Data for a month are typically made available by the 15th of the following month.
What is the difference between the gridded dataset and the index values?
The land and ocean gridded dataset is a large file (~24 mb) that contains monthly temperature anomalies across the globe on a 5 deg x 5 deg grid. The anomalies are calculated with respect to the 1981–2010 base period. Gridded data is available for every month from January 1880 to the most recent month available. You can use it to examine anomalies in different regions of the earth on a month-by-month basis. The index values are an average of the gridded values (see question #7); however, the anomalies are provided with respect to the 20th century (1901–2000) average. They are most useful for tracking the big-picture evolution of temperatures across larger parts of the planet, up to and including the entire global surface temperature.
Global Mean Monthly Surface Temperature Estimates
for the Base Period 1901 to 2000
|1901 to 2000 (°C)||2.8||3.2||5.0||8.1||11.1||13.3||14.3||13.8||12.0||9.3||5.9||3.7||8.5|
|1901 to 2000 (°F)||37.0||37.8||40.8||46.5||52.0||55.9||57.8||56.9||53.6||48.7||42.6||38.7||47.3|
|1901 to 2000 (°C)||15.8||15.9||15.9||16.0||16.3||16.4||16.4||16.4||16.2||15.9||15.8||15.7||16.1|
|1901 to 2000 (°F)||60.5||60.6||60.7||60.9||61.3||61.5||61.5||61.4||61.1||60.6||60.4||60.4||60.9|
|1901 to 2000 (°C)||12.0||12.1||12.7||13.7||14.8||15.5||15.8||15.6||15.0||14.0||12.9||12.2||13.9|
|1901 to 2000 (°F)||53.6||53.9||54.9||56.7||58.6||59.9||60.4||60.1||59.0||57.1||55.2||54.0||57.0|
Please note that the gridded file has been updated to reflect the recent changes in the GHCN-M Temperature Dataset. For more information, please see the GHCN-M version 3.2.0 Technical Report.
To obtain a copy of the monthly average temperature anomalies on a 5° x 5° grid across land and ocean surfaces, please use the following information to access anonymous FTP at NCDC:
Machine Address: ftp.ncdc.noaa.gov
Login Name: anonymous
Password: your email address
Enter: get ncdc-merged-sfc-mntp.dat.gz
For information on the format of the dataset, please visit our Global Historical Climatology Network page. A direct link to the file is also provided on the website.
The Global Anomalies and Index Data
Please Note: Anomalies are provided as departures from the 20th century average (1901-2000).
- The Monthly Global Land Temperature Anomalies (°C)
- The Monthly Global Ocean Temperature Anomalies (°C)
- The Monthly Global (land and ocean combined into an anomaly) Index (°C)
- The Monthly Northern Hemisphere Land Temperature Anomalies (°C)
- The Monthly Northern Hemisphere Ocean Temperature Anomalies (°C)
- The Monthly Northern Hemisphere (land and ocean combined into an anomaly) Index (°C)
- The Monthly Southern Hemisphere Land Temperature Anomalies (°C)
- The Monthly Southern Hemisphere Ocean Temperature Anomalies (°C)
- The Monthly Southern Hemisphere (land and ocean combined into an anomaly) Index (°C)
- The Annual Global Land Temperature Anomalies (°C)
- The Annual Global Ocean Temperature Anomalies (°C)
- The Annual Global (land and ocean combined) Anomalies (°C)
Monthly and annual global anomalies are available through the most recent complete month and year, respectively.
- Peterson, T. C., and R. S. Vose (1997), An Overview of the Global Historical Climatology Network Temperature Database, Bull. Am. Meteorol. Soc., 78, 2837-2849.
- Quayle, R.G., T.C. Peterson, A.N. Basist, and C.S. Godfrey, 1999: An operational near-real-time global temperature index. Geophys. Res. Lett.. 26, 3 (Feb. 1, 1999), 333-335.
- Smith, T. M., and R. W. Reynolds (2004), Improved extended reconstruction of SST (1854-1997), J. Climate, 17, 2466-2477.
- Smith, T. M., and R. W. Reynolds (2005), A global merged land air and sea surface temperature reconstruction based on historical observations (1880-1997), J. Climate, 18, 2021-2036.
- Smith, T. M., et al. (2008), Improvements to NOAA's Historical Merged Land-Ocean Surface Temperature Analysis (1880-2006), J. Climate, 21, 2283-2293.
The complete land-sea surface climatology from the Climate Research Unit is described in:
- Jones, P. D., M. New, D. E. Parker, S. Martin, and I. G. Rigor (1999), Surface Air Temperature and its Changes Over the Past 150 Years, Rev. Geophys., 37(2), 173—199.
Global land areas, excluding Antarctica, described in:
- New, M. G., M. Hulme and P. D. Jones, in press: Representing 20th century space-time climate variability. I: Development of a 1961-1990 mean monthly terrestrial climatology. J. Climate.
Global oceans, 60S-60N, described in:
- Parker, D. E., M. Jackson and E. B. Horton, 1995: The GISST2.2 sea surface temperature and sea-ice climatology. Climate Research Technical Note, CRTN 63, Hadley Centre for Climate Prediction and Research, Bracknel, UK.
Arctic sea areas, described in:
- Rigor, I. G., R. L. Colony and S. Martin, submitted: Statistics of surface air temperature observations in the Arctic. J. Climate.
- Martin, S. and E.A. Munoz: Properties of the Arctic 2-Meter Air temperature field for 1979 to the present derived from a new gridded data set. J. Climate, 10, 1428-1440.