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The historical period (from 1850 to present) yields a window when ice core and good historical data are both available. It thus represents an important period over which to test the relationship between ice core measurements, here stable water isotop
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e96526168fa1a810b83f07192b447276
https://doi.org/10.5194/egusphere-egu22-5847
https://doi.org/10.5194/egusphere-egu22-5847
Stable water isotope ratios are routinely used to infer past climatic conditions in palaeoclimate archives. In particular, oxygen isotope ratios in precipitation co-vary with temperature in high latitudes, and have been established as indicators for
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d652be0e40459278ca27142584a48aad
https://doi.org/10.5194/egusphere-egu2020-19341
https://doi.org/10.5194/egusphere-egu2020-19341
Publikováno v:
Climate of the Past; 2024, Vol. 20 Issue 11, p2539-2560, 22p
Publikováno v:
Hola; 11/6/2024, Vol. 4 Issue 188, p78-78, 1/2p, 2 Color Photographs