Changes

People measure modern temperature records using instruments. Records only cover the last 150 years or so. The '''temperature record of the past 1,000 years''' or more is found by using data from what are called "climate proxy" records.  

People measure modern temperature records using instruments. Records only cover the last 150 years or so. The '''temperature record of the past 1,000 years''' or more is found by using data from what are called "climate proxy" records.  

Proxies can be anything which relates to climate. Short term [[autobiographies]] often talk about the weather in past eras, and we do have some autobiographies from 2000 years ago. There are also [[tree rings]] and other methods which go back about 20,000 years. Further back still, there is evidence from geology, the record of the rocks. However, this page is just about the last 1000 years.<ref>Jones P.D; Briffa K.R; Barnett T.P. & Tett S.F.B. 1998, High-resolution palaeoclimatic records for the last millennium: interpretation, integration and comparison with General Circulation Model control-run temperatures, ''The Holocene'', '''8''' (4): 455–471. [https://journals.sagepub.com/doi/10.1191/095968398667194956]</ref><ref>Mann M.E; Bradley R.S. & Hughes M.K. 1999. Northern hemisphere temperatures during the past millennium: inferences, uncertainties, and limitations. ''Geophysical Research Letters'' '''26''' (6): 759–762. [https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/1999GL900070]</ref>

Proxies can be anything which relates to climate. Short term [[autobiographies]] often talk about the weather in past eras, and we do have some autobiographies from 2000 years ago. There are also [[tree rings]] and other methods which go back about 20,000 years. Further back still, there is evidence from geology, the record of the rocks. However, this page is just about the last 1000 years.<ref>Jones P.D; Briffa K.R; Barnett T.P. & Tett S.F.B. 1998, High-resolution palaeoclimatic records for the last millennium: interpretation, integration and comparison with General Circulation Model control-run temperatures, ''The Holocene'', '''8''' (4): 455–471. [https://journals.sagepub.com/doi/10.1191/095968398667194956]</ref><ref>Mann M.E; Bradley R.S. & Hughes M.K. 1999. Northern hemisphere temperatures during the past millennium: inferences, uncertainties, and limitations. ''Geophysical Research Letters'' '''26''' (6): 759–762. [https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/1999GL900070] {{Webarchive|url=https://web.archive.org/web/20191210203035/https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/1999GL900070 |date=2019-12-10 }}</ref>

We are fairly sure there was a warm period about 1,000 years ago, and a cold period about the 17th century. Even in the 19th century people skated on the [[Thames]] in wintertime.

We are fairly sure there was a warm period about 1,000 years ago, and a cold period about the 17th century. Even in the 19th century people skated on the [[Thames]] in wintertime.