Ice Age () - IMDb
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Discussion and conclusions In this study evidence for 'classic' late Little Ice Age activity was observed at nine glaciers along the Beagle Channel on the southside of the Cordillera Darwin. Preliminary data from Glaciar Italia shows that its outermost moraine was deposited between AD and AD, with the latter date considered a more accurate age.
At each of the other observed glacier forefields similar evidence is visible in the form of distinct breaks in the forest cover, especially between the mature forest cover outside the moraines and the forest cover inside the glacier forefield. On air photos and satellite scenes of Cordillera Darwin similar landforms and vegetation breaks seem to be present for most glaciers including glaciers on the north, west, and east sides, indicating that glaciers of Cordillera Darwin advanced during the late Little Ice Age.
This contrasts with the findings of more recent studies and needs explanation. The calibrated range of the BP date is AD 1 sigma or AD 2 sigmaand for both sigma ranges there is a very low possibility, 0.
The potential problem with young radiocarbon dates is well known Porter, This means the site could have been icefree as early as the late 15th century, but it also could have been icefree only since the early 19th century. Nonetheless, Kuylenstierna et al. However, the site of the BP date is about 3. Even if the site was icefree at its earliest calibrated time, it is possible that the glacier reached well beyond the site, as the site is m above sea level, and thus the glacier could have thickened and advanced but stayed below the site.
Ventisquero Garibaldi started to advance in until at least October for over 1. However, at Evangelistas Fig. Some of the glaciers that have remained stable or advanced are calving glaciers, and thus some authors argue that they might not record climatic conditions Warren, They argue that increased wind activity could account for windward glaciers to advance due to increased orographic precipitation, and leeward glaciers to retreat significantly due to fohn winds, as observed at Ventisquero Marinelli Fig.
Some glaciers in New Zealand and Norway also advanced at the end of the 20th century Chinn et al. In maritime Norway advances started as early as the mids, but were pronounced from the mids until around In New Zealand advances lasted from the mids to around They conclude that an increase in the strength of the westerly circulation and an associated increase in precipitation can explain the glacier advances in New Zealand and Norway.
The Southern Annular Mode, a measure of zonal pressure gradient between S and S, showed a positive trend between the mids to Marshall et al. It thus appears that similar to glaciers in Norway and New Zealand, an increase of westerly airflow and an associated significant increase in precipitation apply to some maritime glaciers of the Cordillera Darwin, and that those conditions can offset increases in temperature, which could explain glacier behaviour on the windward side.
References Cited Aniya, M. Arctic, Antarctic, and Alpine Research, 31, Reconstructing climate variability in southern Chilean Andes. Spatio-temporal rainfall patterns in southern South America. International Journal of Climatology, 29, Recent glacier advances in Norway and New Zealand: A comparison of their glaciological and meteorological causes.
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Geografiska Annaler, 87A, Twentieth century climate change: Proceedings of the National Academy of Sciences, 97, The Little Ice Age.
Anomalous glacier responses to 20th century climatic changes in Darwin Cordillera, southern Chile. Journal of Glaciology, 41, Glacier and lake-level variations in west-central Europe over the last years. The Holocene, 15, Improving age estimates for late Holocene glacial landforms using dendrochronology - some examples from Garibaldi Provincial Park.
Quaternary Geochronology, 4, Canadian Journal of Earth Sciences, 44, The Holocene, 6, Nieves and glaciares de Chile: Ediciones de la Universidad de Chile, Santiago de Chile. Assessing the synchroneity of glacier fluctuations in the western Cordillera of the Americas during the last millenium.
Interhemspheric Climate Linkages pp. Academic Press, New York.
Ice Age () - Release Info - IMDb
Fluctuations of the South Patagonian Icefield during the last glaciation and the Holocene. Journal of Quaternary Science, 10, Causes of exceptional atmospheric circulation changes in the Southern Hemisphere. Geophysical Research Letters, 31, L Palaeogeography, Palaeoclimatology, Palaeoecology, Glacier fluctuations in extratropical South America during the past years. Quaternary Research, 73, Patagonian glacier advances in concert with those in western North America.
Sampling height-age error correction for spruce seedlings in glacial forefield, Canadian Cordillera. Arctic and Alpine Research, 23, Estimating ecesis for tree-ring dating of moraines: A comparative study from the Canadian Cordillera.
Arctic and Alpine Research, 25, Variations of some Patagonian glaciers since the Late-Glacial. American Journal of Science, Variations of some Patagonian glaciers since the Late-Glacial: Annals of Glaciology, 56, Glacier change and climate forcing in recent decades at Gran Campo Nevado, southernmost Patagonia. Annals of Glaciology, 46, Extracting a climate signal from glacier records. Anales del Instituto de la Patagonia, 31, Glaciological evidence of Holocene climatic change.
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Cambridge University Press, Cambridge. Contribution of the Patagonia Icefields of South America to sea level rise. Recent climatic changes in western Patagonia. Bulletin of Glacier Research, 13, Recent temperature variations in southern South America.
International Journal of Climatology, 17, Here's what she had to say. This interview was edited ds condensed for clarity.
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