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[PDF] Top 20 Windiness spells in SW Europe since the last glacial maximum

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Windiness spells in SW Europe since the last glacial maximum

Windiness spells in SW Europe since the last glacial maximum

... ages. The entire dataset includes 24 OSL ages from the explored transgressive dunefield ...(i.e. the cliff-top dune and the inland dunefield). The peaks represent discrete phases of ... See full document

33

Territoriality and the organization of technology during the Last Glacial Maximum in southwestern Europe

Territoriality and the organization of technology during the Last Glacial Maximum in southwestern Europe

... with the expectations presented since they result from a com- plex interplay among patterns of inheritance, interaction, and local ...and the restricted options inherent to leptolithic technologies ... See full document

32

Adaptation to Resources and Environments during the Last Glacial Maximum by Hunter-Gatherer Societies in Atlantic Europe

Adaptation to Resources and Environments during the Last Glacial Maximum by Hunter-Gatherer Societies in Atlantic Europe

... Once the nodes of the network are defined, the edges (i.e., the links between sources and discard areas) can be defined in two ...However, since movement is constrained by ... See full document

20

Bioclimatic modeling in the Last Glacial Maximum, Mid-Holocene and facing future climatic changes in the strawberry tree (Arbutus unedo L.)

Bioclimatic modeling in the Last Glacial Maximum, Mid-Holocene and facing future climatic changes in the strawberry tree (Arbutus unedo L.)

... to the Mediterranean region and Western Europe, and belongs to the Ericaceae family and to sclerophyllous and laurel-like ...flora. The species’ distribution is mainly throughout areas where ... See full document

16

Braz. j. oceanogr.  vol.57 número2

Braz. j. oceanogr. vol.57 número2

... with the modern coastal drainage ...that the sea-level rise rate and the posterior marine erosion/deposition may have more influence on the size and shape of the drowned channels than ... See full document

9

Sea ice led to poleward-shifted winds at the Last Glacial Maximum: the influence of state dependency on CMIP5 and PMIP3 models

Sea ice led to poleward-shifted winds at the Last Glacial Maximum: the influence of state dependency on CMIP5 and PMIP3 models

... apparent glacial to interglacial wind change results (Liu et ...of the bound- ary layer, this can lead to quite different results for glacial to interglacial changes in different wind ... See full document

13

Migrating subtropical front and Agulhas Return Current affect the southwestern Indian Ocean during the late Quaternary

Migrating subtropical front and Agulhas Return Current affect the southwestern Indian Ocean during the late Quaternary

... 1. The location of core SK 200/17 is marked with a black filled square. The surface circula- tion in this region, which includes South Equatorial Current (SEC), Mozambique Channel (MC), East ... See full document

31

Changes in atmospheric variability in a glacial climate and the impacts on proxy data: a model intercomparison

Changes in atmospheric variability in a glacial climate and the impacts on proxy data: a model intercomparison

... to the possibility of comparing model simulations with proxy-based observations when and where these are ...during the mid- Holocene (6000 yrs before present, 6 ka) warm interval, the atmosphere ... See full document

14

Sediment core fossils in ancient Lake Ohrid: testing for faunal change since the Last Interglacial

Sediment core fossils in ancient Lake Ohrid: testing for faunal change since the Last Interglacial

... cores in Lake Ohrid reported here opens a whole new perspective on evolutionary research in this famous ancient lake in par- ticular, and to interdisciplinary research resulting from lake drilling ... See full document

12

Impacts of land surface properties and atmospheric CO<sub>2</sub> on the Last Glacial Maximum climate: a factor separation analysis

Impacts of land surface properties and atmospheric CO<sub>2</sub> on the Last Glacial Maximum climate: a factor separation analysis

... with the climatic reconstructions of Wu et al. (2007) over Europe and Western Siberia, notably due to the inclusion of vege- tation ...well the south-west to north-east MTCO gradient from ... See full document

20

A 33,000-year-old incipient dog from the Altai Mountains of Siberia: evidence of the earliest domestication disrupted by the Last Glacial Maximum.

A 33,000-year-old incipient dog from the Altai Mountains of Siberia: evidence of the earliest domestication disrupted by the Last Glacial Maximum.

... of the Razboinichya canid were measured (see Tables S1, S2) according to standard osteological criteria ...[13]. The skull and both mandibles were also photo- graphed with cm scale from several perspectives ... See full document

7

Quantitative reconstruction of precipitation changes on the NE Tibetan Plateau since the Last Glacial Maximum &amp;ndash; extending the concept of pollen source-area to pollen-based climate reconstructions from large lakes

Quantitative reconstruction of precipitation changes on the NE Tibetan Plateau since the Last Glacial Maximum &ndash; extending the concept of pollen source-area to pollen-based climate reconstructions from large lakes

... during the Late Glacial and the Holocene, provides an indispensable key to predicting future climatic ...change, the Tibetan Plateau has become a focus for several palaeoclimatological studies ... See full document

51

Quantifying the roles of ocean circulation and biogeochemistry in governing ocean carbon-13 and atmospheric carbon dioxide at the last glacial maximum

Quantifying the roles of ocean circulation and biogeochemistry in governing ocean carbon-13 and atmospheric carbon dioxide at the last glacial maximum

... to the large increase in dust iron supply, which results from phytoplank- ton physiological and ocean circulation ...that the OGCBM primary productivity response to the ad- ditional dust iron ... See full document

12

Corrigendum to &quot;Quantitative reconstruction of precipitation changes on the NE Tibetan Plateau since the Last Glacial Maximum &amp;ndash; extending the concept of pollen source area to pollen-based climate reconstructions from large lakes&quot; published in Clim.

Corrigendum to "Quantitative reconstruction of precipitation changes on the NE Tibetan Plateau since the Last Glacial Maximum &ndash; extending the concept of pollen source area to pollen-based climate reconstructions from large lakes" published in Clim.

... After the above mentioned paper was published, we realized that the description of our statistical method (PROTEST) has a little mistake because it is not a block resampling method as we stated in ... See full document

1

Reconstructing glacier-based climates of LGM Europe and Russia &amp;ndash; Part 3: Comparison with GCM and pollen-based climate reconstructions

Reconstructing glacier-based climates of LGM Europe and Russia &ndash; Part 3: Comparison with GCM and pollen-based climate reconstructions

... and glacial-geological LGM climate anomalies (Allen et ...shown in the left hand graphs and the colour of these bars can be used to identify the regional temperature anomalies in ... See full document

35

Mining Interesting Patterns and Rules in a Time-evolving Graph

Mining Interesting Patterns and Rules in a Time-evolving Graph

... Recently, the study of human activities on social and communication networks attract a large amount of ...attention. In general, patterns on local structures in those networks can provide useful ... See full document

6

Monarchy, Empire, and Popular Politics in the Atlantic Age of Revolutions

Monarchy, Empire, and Popular Politics in the Atlantic Age of Revolutions

... of the work of the authors in this dossier yields at least four conclusions about the current state of the ...First, the studies continue to provide irrefutable evidence about ... See full document

21

Simulating the vegetation response in western Europe to abrupt climate changes under glacial background conditions

Simulating the vegetation response in western Europe to abrupt climate changes under glacial background conditions

... given the relatively coarse resolution of our model. Given the duration of our experiment, which is short compared to the time resolution of most of the available pollen records, our results ... See full document

22

Climate history of the Southern Hemisphere Westerlies belt during the last glacial-interglacial transition revealed from lake water oxygen isotope reconstruction of Laguna Potrok Aike (52° S, Argentina)

Climate history of the Southern Hemisphere Westerlies belt during the last glacial-interglacial transition revealed from lake water oxygen isotope reconstruction of Laguna Potrok Aike (52° S, Argentina)

... for the sediment section between 9 and 20 m event-corrected com- posite depth (cd-ec) from the composite profile 5022-2CP of Laguna Potrok Aike ...details). The age-depth model used in ... See full document

49

Evaluating signatures of glacial refugia for North Atlantic benthic marine taxa

Evaluating signatures of glacial refugia for North Atlantic benthic marine taxa

... particularly the one culminating in the Last Glacial Maximum ;21 ka (thousands of years ago), greatly affected the distributions and population sizes of temperate marine ... See full document

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