How the climate drives sea-level changes
نویسندگان
چکیده
منابع مشابه
Holocene paleoecology along the Blekinge coast, southeast Sweden, and implications for climate and sea-level changes
To investigate the Holocene vegetation history and shoreline displacement along the southeastern Swedish coast, two radiocarbon dated pollen, macrofossil, and mineral magnetic sequences were studied in the western Blekinge coast: Hunnemara Lake and Smygen Bay. Both pollen records show mosaic vegetation with grasslands, heaths and woodlands prior to 11,300 cal. BP. Pinus-dominated mixed forest w...
متن کاملSedimentological evidence of the level and climate changes of Lake Zeribar in the Holocene
Lakes are very interesting sedimentary environments for the study of ancient climate, changes in sedimentary environments and lake level changes. Lake Zeribar is situated in the Zagros Mountains, Kurdistan, Iran. The main purpose of this research is to examine grain size sediments, geochronology and clay mineralogy accumulated in Zeribar Lake in order to check the water level fluctuations, clim...
متن کاملClimate Change: The Impacts of Sea Level Rise on Egypt
Introduction Sea level changes are caused by several natural phenomenon; the three primary contributing ones are: ocean thermal expansion, glacial melt from Greenland and Antarctica (plus a smaller contribution from other ice sheets), and change in terrestrial storage. Among those, ocean thermal expansion has been expected to be the dominating factor behind the rise in sea level. However, new d...
متن کاملClimate Change: The Impacts of Sea Level Rise on Egypt
Introduction Sea level changes are caused by several natural phenomenon; the three primary contributing ones are: ocean thermal expansion, glacial melt from Greenland and Antarctica in addition to a smaller contribution from other ice sheetsand change in terrestrial storage. Among those, ocean thermal expansion has been expected to be the dominating factor behind the rise in sea level. However,...
متن کاملClimate related sea-level variations over the past two millennia.
We present new sea-level reconstructions for the past 2100 y based on salt-marsh sedimentary sequences from the US Atlantic coast. The data from North Carolina reveal four phases of persistent sea-level change after correction for glacial isostatic adjustment. Sea level was stable from at least BC 100 until AD 950. Sea level then increased for 400 y at a rate of 0.6 mm/y, followed by a further ...
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ژورنال
عنوان ژورنال: Astronomy & Geophysics
سال: 2008
ISSN: 1366-8781,1468-4004
DOI: 10.1111/j.1468-4004.2008.49224.x