JMA estimates global temperature anomalies using data combined not only over land but also over ocean areas.
The land part of the combined data for the period before 2000 consists of GHCN (Global Historical Climatology Network) information provided by NOAA (The National Oceanic and Atmospheric Administration), while that for the period after 2001 consists of CLIMAT messages archived at JMA.
The oceanic part of the combined data consists of JMA's own long-term sea surface temperature analysis data, known as COBE-SST (see the articles in TCC News No.1 and this report).
The procedure for estimating the global mean temperature anomaly is outlined below.
1) An average is obtained for monthly-mean temperature anomalies against the 1971-2000 baseline over land in each 5° x 5° grid box worldwide.
2) An average is obtained for monthly mean sea surface temperature anomalies against the 1971-2000 baseline in each 5° x 5° grid box worldwide in which at least one in-situ observation exists. SST anomalies in regions covered by ice are not used.
3) An average is obtained for the values in 1) and 2) according to the land-to-ocean ratio for each grid box.
4) Monthly mean global temperature anomaly is obtained by averaging the anomalies of all the grid boxes weighted with the area of the grid box.
5) Annual and seasonal mean global temperature anomalies are obtained by averaging monthly-mean global temperature anomalies.
6) The baseline period is adjusted to 1981-2010.
Image: average of temperature anomalies over land and sea according to the land-to-ocean ratio for each grid box[Global Temperature Top]