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Global surface temperature (GST) is the average temperature of Earth's surface at a given time. It is a combination of sea surface temperature and the near-surface air temperature over land, weighted by their respective areas. Temperature data comes mainly from weather stations and satellites. To estimate data in the distant past, proxy data can be used…
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temperature global temperatures climate years surface records data ice land period changes warming average time record ocean change since used
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| from tree rings | instance of | Instrumental temperature records do not use indirect reconstructions using climate proxy data | 0.80 | text |
| marine sediments.Early temperature recordsThe longest-running temperature record is the Central England temperature data series | instance of | Instrumental temperature records do not use indirect reconstructions using climate proxy data | 0.80 | text |
| a single-location data set that starts in 1659.On 15 December 2025 | instance of | Instrumental temperature records do not use indirect reconstructions using climate proxy data | 0.80 | text |
| the Copernicus Programme's Earth System Science Data released the GloSAT reference analysis | instance of | Instrumental temperature records do not use indirect reconstructions using climate proxy data | 0.80 | text |
| a gridded data set of air temperature change across global land | instance of | Instrumental temperature records do not use indirect reconstructions using climate proxy data | 0.80 | text |
| ocean extending back to the 1780s | instance of | Instrumental temperature records do not use indirect reconstructions using climate proxy data | 0.80 | text |
| using marine air temperature observations rather than the sea surface temperature measurements.Before GloSAT's release | instance of | Instrumental temperature records do not use indirect reconstructions using climate proxy data | 0.80 | text |
| the period for which reasonably reliable instrumental records of near-surface land temperature exist with quasi-global coverage was generally considered to begin around 1850 | instance of | Instrumental temperature records do not use indirect reconstructions using climate proxy data | 0.80 | text |
| a Stevenson screen | instance of | with the instruments being sheltered from direct sunlight using a shelter | 0.80 | text |
| polar regions | instance of | temperature observations are more spread out in sparsely populated areas | 0.80 | text |
| deserts | instance of | temperature observations are more spread out in sparsely populated areas | 0.80 | text |
| as well as in many regions of Africa | instance of | temperature observations are more spread out in sparsely populated areas | 0.80 | text |
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