Little Ice Age advance and retreat of Glaciar Jorge Montt, Chilean Patagonia
نویسندگان
چکیده
منابع مشابه
Little ice age advance and retreat of Glaciar Jorge Montt, Chilean Patagonia
Introduction Conclusions References
متن کاملLittle Ice Age
Volume 1, The Earth system: physical and chemical dimensions of global environmental change, pp 504–509
متن کاملRapid viscoelastic uplift in southeast Alaska caused by post-Little Ice Age glacial retreat
Our observations show that extreme uplift in southeast Alaska began about 1770 AD, with relative sea level (RSL) change to 5.7 m and current uplift rates to 32 mm/yr. This region experienced widespread glacial melting following the Little Ice Age (LIA), with the collapse of the Glacier Bay Icefield alone equivalent to 8 mm of global sea level rise. Geodynamic modelling links the uplift to post-...
متن کاملVarve and radiocarbon dating support the rapid advance of Jakobshavn Isbr during the Little Ice Age
Large outlet glaciers draining the Greenland Ice Sheet significantly influence overall ice sheet mass balance. Considerable short term (years to decades) retreat and fluctuations in velocity of Jakobshavn Isbræ, western Greenland, illustrate the complex nature by which large outlet glaciers respond to climate change, making predictions of future ice sheet change challenging. To provide a longer...
متن کاملIce-atmosphere interactions during sea-ice advance and retreat in the western Antarctic Peninsula region
[1] The seasonal evolution of sea-ice extent, concentration, and drift in the western Antarctic Peninsula (WAP) region, along with regional atmospheric synoptic variability, are described for a winter period (1992) when sea-ice advance and retreat were both anomalously early. Daily time series of winds, opening and closing of the sea-ice cover, and volume fluxes in and out of the WAP region ind...
متن کاملذخیره در منابع من
با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید
ژورنال
عنوان ژورنال: Climate of the Past
سال: 2012
ISSN: 1814-9332
DOI: 10.5194/cp-8-403-2012