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Odonate Diversity Patterns in Italy Disclose Intricate Colonization Pathways
As a natural bridge between Europe and Africa, Italy occupies a prominent position to understand the biogeography of Europe. The influence of climatic, spatial, and historical factors on current patterns of species richness and turnover (i.e., inter ...
Simone Fattorini
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Impending ice age of assisted reproductive technology [PDF]
Pietro Bortoletto, M.D.
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Multidecadal Arctic sea ice thickness and volume derived from ice age [PDF]
Sea ice is a key component of the Arctic climate system, and has impacts on global climate. Ice concentration, thickness, and volume are among the most important Arctic sea ice parameters.
Y. Liu, J. R. Key, X. Wang, M. Tschudi
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A one-dimensional temperature and age modeling study for selecting the drill site of the oldest ice core near Dome Fuji, Antarctica [PDF]
The recovery of a new Antarctic ice core spanning the past ∼ 1.5 million years will advance our understanding of climate system dynamics during the Quaternary.
T. Obase +12 more
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Digital portrait of state and variability for the ice cover of Japan Sea
Seasonal and long-term variability of the ice age and concentration in the Japan Sea is analyzed on the base of all available information for 1960–2019.
S. I. Kislova +2 more
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Methodology for determining climate change by analysis of impurity concentrations in the glacier
The work contains the analysis of possible distributions of aerosol impurities through the glacier depth in those regions of Antarctica, where synoptic maps have shown stabilization of cyclones; and based on this analysis a methodology has been proposed ...
M. D. Curmei +3 more
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Variability of Arctic Sea ice age and its relationship with atmospheric circulation patterns
Since at least the 1990s, global warming has caused the decline of multi-year ice (MYI) in the Arctic, which has made the Arctic Ocean more susceptible to the effects of climate change and weather processes.
Ping Chen +7 more
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The Ice Core Gas Age‐Ice Age Difference as a Proxy for Surface Temperature
Ice cores provide detailed records of past climate change. Water stable isotopes are the most commonly used ice core climate proxy, but their quantitative interpretation remains challenging.
Christo Buizert
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Glacial retreat from the North Cascade Range after the Last Glacial Maximum (LGM) at approximately 21 ka until the end of the Pleistocene at 11.6 ka was complex and included both continental and alpine glaciers.
J.L. Riedel
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