Results 261 to 270 of about 416,494 (310)
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Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences, 2003
Understanding the mechanisms of past climate changes requires modelling of the complex interaction between all major components of the Earth system: atmosphere, ocean, cryosphere, lithosphere and biosphere. This paper reviews attempts at such an integrative approach to modelling climate changes during the glacial age.
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Understanding the mechanisms of past climate changes requires modelling of the complex interaction between all major components of the Earth system: atmosphere, ocean, cryosphere, lithosphere and biosphere. This paper reviews attempts at such an integrative approach to modelling climate changes during the glacial age.
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Late-glacial and early post-glacial Scotland
Proceedings of the Society of Antiquaries of Scotland, 1937openaire +1 more source
Southern Ocean glacial conditions and their influence on deglacial events
Nature Reviews Earth & Environment, 2023Elisabeth L Sikes, Thomas Williams
exaly
Measuring glacial lake bathymetry using uncrewed surface vehicles
Nature Reviews Earth & Environment, 2023Menger Peng
exaly
1991
Abstract Today, glaciers cover 10 percent of the Earth’s land area, whereas 30 percent was covered during the maximum glaciation of the Quaternary Period. Although 20 percent of the Earth’s surface has a direct glacial heritage, another 12 percent was impacted by glacially related climates and sediments.
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Abstract Today, glaciers cover 10 percent of the Earth’s land area, whereas 30 percent was covered during the maximum glaciation of the Quaternary Period. Although 20 percent of the Earth’s surface has a direct glacial heritage, another 12 percent was impacted by glacially related climates and sediments.
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Fennoscandia: glacial landforms from the Last Glacial Maximum
2022Greenwood, S. L., Hughes, Anna L.C.
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