Modeling ocean–atmosphere carbon budgets during the Last Glacial Maximum–Heinrich 1 meltwater event–Bølling transition

2000 ◽  
Vol 90 (2) ◽  
pp. 412-425 ◽  
Author(s):  
M. Schulz ◽  
D. Seidov ◽  
M. Sarnthein ◽  
K. Stattegger
Keyword(s):  
Last Glacial Maximum ◽  
Glacial Maximum ◽  
Carbon Budgets ◽  
Last Glacial ◽  
Ocean Atmosphere ◽  
The Last Glacial Maximum ◽  
The Last Glacial

Impact of a realistic river routing in coupled ocean–atmosphere simulations of the Last Glacial Maximum climate

2007 ◽  
Vol 30 (7-8) ◽  
pp. 855-869 ◽  
Author(s):  
Ramdane Alkama ◽  
M. Kageyama ◽  
G. Ramstein ◽  
O. Marti ◽  
P. Ribstein ◽  
...  
Keyword(s):  
Last Glacial Maximum ◽  
Glacial Maximum ◽  
Last Glacial ◽  
Ocean Atmosphere ◽  
The Last Glacial Maximum ◽  
Last Glacial Maximum Climate ◽  
The Last Glacial ◽  
River Routing

scholarly journals Northern hemisphere storm tracks during the last glacial maximum in the PMIP2 ocean-atmosphere coupled models: energetic study, seasonal cycle, precipitation

2008 ◽  
Vol 32 (5) ◽  
pp. 593-614 ◽  
Author(s):  
A. Laîné ◽  
M. Kageyama ◽  
D. Salas-Mélia ◽  
A. Voldoire ◽  
G. Rivière ◽  
...  
Keyword(s):  
Last Glacial Maximum ◽  
Northern Hemisphere ◽  
Seasonal Cycle ◽  
Glacial Maximum ◽  
Storm Tracks ◽  
Coupled Models ◽  
Last Glacial ◽  
Ocean Atmosphere ◽  
The Last Glacial Maximum ◽  
The Last Glacial

Estimating the carbon transfer between the ocean, atmosphere and the terrestrial biosphere since the last glacial maximum

Terra Nova ◽  
1995 ◽  
Vol 7 (3) ◽  
pp. 358-366 ◽  
Author(s):  
M.A. Maslin ◽  
J. Adams ◽  
E. Thomas ◽  
H. Faure ◽  
R. Haines‐Young
Keyword(s):  
Last Glacial Maximum ◽  
Glacial Maximum ◽  
Terrestrial Biosphere ◽  
Last Glacial ◽  
Carbon Transfer ◽  
Ocean Atmosphere ◽  
The Last Glacial Maximum ◽  
The Last Glacial

Continental/Cordilleran ice interactions: a dominant cause of westward super-elevation of the last glacial maximum continental ice limit in southwestern Alberta, Canada

2001 ◽  
Vol 30 (1) ◽  
pp. 43-52 ◽  
Author(s):  
Edward C. Little ◽  
Lionel E. Jackson ◽  
Thomas S. James ◽  
Stephen R. Hicock ◽  
Elizabeth R. Leboe
Keyword(s):  
Last Glacial Maximum ◽  
Glacial Maximum ◽  
Last Glacial ◽  
The Last Glacial Maximum ◽  
The Last Glacial

Mollusk record of millennial climate variability in the Loess Plateau during the Last Glacial Maximum

Boreas ◽  
2002 ◽  
Vol 31 (1) ◽  
pp. 20-27 ◽  
Author(s):  
Naiqin Wu ◽  
Tungsheng Liu ◽  
Xiuping Liu ◽  
Zhaoyan Gu
Keyword(s):  
Climate Variability ◽  
Last Glacial Maximum ◽  
Loess Plateau ◽  
Glacial Maximum ◽  
The Loess Plateau ◽  
Last Glacial ◽  
The Last Glacial Maximum ◽  
The Last Glacial

Reconstructions of the past distribution of Testudo graeca mitochondrial lineages in the Middle East and Transcaucasia support multiple refugia since the Last Glacial Maximum

2021 ◽  
pp. 10-17
Author(s):  
Oguz Turkozan
Keyword(s):  
Middle East ◽  
Last Glacial Maximum ◽  
Glacial Maximum ◽  
Testudo Graeca ◽  
Last Glacial ◽  
The Past ◽  
Precipitation Seasonality ◽  
Multiple Refugia ◽  
The Last Glacial Maximum ◽  
The Last Glacial

A cycle of glacial and interglacial periods in the Quaternary caused species’ ranges to expand and contract in response to climatic and environmental changes. During interglacial periods, many species expanded their distribution ranges from refugia into higher elevations and latitudes. In the present work, we projected the responses of the five lineages of Testudo graeca in the Middle East and Transcaucasia as the climate shifted from the Last Glacial Maximum (LGM, Mid – Holocene), to the present. Under the past LGM and Mid-Holocene bioclimatic conditions, models predicted relatively more suitable habitats for some of the lineages. The most significant bioclimatic variables in predicting the present and past potential distribution of clades are the precipitation of the warmest quarter for T. g. armeniaca (95.8 %), precipitation seasonality for T. g. buxtoni (85.0 %), minimum temperature of the coldest month for T. g. ibera (75.4 %), precipitation of the coldest quarter for T. g. terrestris (34.1 %), and the mean temperature of the driest quarter for T. g. zarudyni (88.8 %). Since the LGM, we hypothesise that the ranges of lineages have either expanded (T. g. ibera), contracted (T. g. zarudnyi) or remained stable (T. g. terrestris), and for other two taxa (T. g. armeniaca and T. g. buxtoni) the pattern remains unclear. Our analysis predicts multiple refugia for Testudo during the LGM and supports previous hypotheses about high lineage richness in Anatolia resulting from secondary contact.

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