«The authors write that «the Mediterranean region is one of the world's most vulnerable areas with respect to global warming,»... they thus consider it to be extremely important to determine what impact further temperature increases might have on the storminess of the region... produced a high - resolution record of paleostorm events along the French Mediterranean coast over the past 7000 years... from the sediment bed of Pierre Blanche Lagoon [near Montpellier, France]... nine French scientists, as they describe it, «recorded seven periods of increased storm activity at 6300 - 6100, 5650 - 5400, 4400 - 4050, 3650 - 3200, 2800 - 2600, 1950 - 1400, and 400 - 50
cal yr BP,» the latter of which intervals they associate with the Little Ice Age.
The HIM ended with a temperature drop at 3500 - 2500
cal yr BP associated with permafrost initiation in the region.
Our records suggest that the early - Holocene summer temperatures from 11,500
cal yr BP onwards were already slightly higher than at present, followed by a stable Holocene Thermal Maximum (HTM) at 8000 - 3500
cal yr BP when summer temperatures in the tundra were ca. 3 degrees C above present - day values.
Mixed spruce forest began to disappear around lake Kharinei at ca. 3500
cal yr BP, with the last tree macrofossils recorded at ca. 2500
cal yr BP.
Blarquez et al., 2018 Magyari et al., 2018... its climatic tolerance limits were used to infer July mean temperatures exceeding modern values by 2.8 °C at this time [8200 - 6700
cal yr BP](Magyari et al., 2012).
Abstract: «Times of major transitions identified in pollen records occurred at 600, 1650, 2850, 4030, 6700, 8100, 10 190, 12 900, and 13 800
cal yr B.P., consistent with ice and marine records.
â $ œIntervals of ameliorated limnological conditions occurred between 1300 and 900 and between 500 and 280
cal yr B.P., briefly interrupting the decreasing trend in productivity that culminated in the Little Ice Age.
The oldest bone was dated at approximately 6,400
cal yr BP, several thousand years after humans colonized the islands.
The results suggest storminess increased after 1000
cal yrs BP, with higher storminess during the Medieval Climate Anomaly (MCA) than the LIA, supporting the hypothesis that the NAO - storminess relationship was consistent with the instrumental period.
Not exact matches
yr BP (OZM148; 235 cm) and 13,890 ± 140
cal.
yr BP (OZM149; 292 cm depth) to 13,590 ± 160
cal.
Im
cal im 46 im a cree frm wabasca I dnt dribk or do any drugs im wrk full tyme at bigstone health commision past 7
yrs mainrance im easy goin guy like doin familyevents outdoors lik goin to family events roundance or powows wen ever I have tyme
Assuming a 10 degree temperature difference between the temperature of the runoff and the average temperature of the ocean that would be 5 * 10 ^ 18
cal or 2 * 10 ^ 19 J /
yr.
yr B.P., but reformed by ca. 7945
cal.
yr BP, however, spruce cover decreased steadily from an average of 35 % at 2200
cal.
yr BP to 20 % at 900
cal.
yr BP corresponds to possible start - up of rapid deforestation, assuming that fire activity from 900 to 600
cal.