Holocene vegetation and biomass changes on the Tibetan Plateau – a model-pollen data comparison

Modern pollen samples collected from di ff erent parts of Lake Donggi Cona (in the north-eastern part of the Tibetan Plateau) reveal variations in pollen assemblages within this

For the organic carbon storage in 0–1 m depth, the reported SOC densities data of 190 sampling sites were collected through their distribution in permafrost regions (Fig.. The area

ment. The robustness of the simulations is also tested by comparison with two previous simulations of European MHL vegetation. We then try and isolate the climate factors driving

A significant build-up of air pollution during the 13– 19 March 2009 event was also observed at stations in the IGP and in northern Thailand. Measurements of AERONET sites

The intercomparison experiments show that the Pit gauge caught 1 % more rainfall, 2 % more mixed precipitation, 4 % less snowfall and 0.8 % more precipitation (all types) than the

simulations are utilized to explain and explore di ff erences in the soil moisture response due to di ff erent vegetation types and their impact on the temporal variability of

The summer precipitation in Southeast Asia (Fig. 1g) increases rapidly dur- ing the early to mid-Holocene (9 kyr BP to 6 kyr BP) with the gradually increased snow and glacier cover

In addition, the two deep permafrost sites in the Heihe River Basin (Heihe-1, Heihe-2) were the alpine meadow and rich in organic carbon with high soil water contents (Mu et