This paper describes the general moisture conditions and the annual and seasonal trends of temperature, precipitation, potential evapotranspiration and aridity/humidity index from 1971 to 2000 in China. Observed climatic data from 616 meteorological stations over China's land surface were used. Pote
The variation of moisture conditions in China during the last 2000 years
β Scribed by Gaofa Gong; Sultan Hameed
- Publisher
- John Wiley and Sons
- Year
- 2007
- Tongue
- English
- Weight
- 783 KB
- Volume
- 11
- Category
- Article
- ISSN
- 0899-8418
No coin nor oath required. For personal study only.
β¦ Synopsis
Abstract
Utilizing more than 50,000 reports of droughts and floods found in local records we have reconstructed the history of moisture conditions in eastern China for the last 2000 years. The area studied extends eastward of Gansu province and is situated between Inner Mongolia in the north and Zhejiang in the south. Separate analyses are presented for the semiβarid, semiβwet and wet subdivisions of this area. It was possible to develop moisture indices with a time resolution of 5 years in each subregion. The time series of the moisture index presented for the semiβwet area extends over the period AD 1β1950, while for the other two subregions the period covered is AD 251β1950.
Each of the climatic subdivisions is found to undergo prolonged periods of dryness and wetness. The frequency of alternation between dry and wet conditions increases from the semiβarid region to the semiβwet region to the wet region. The variations of moisture conditions in the whole area of eastern China is compared with known changes in the level of the Caspian Sea. The variations in the two regions are found to be coherent.
π SIMILAR VOLUMES
The sedimentary succession of piston core RC26-16, dated by 14 C accelerator mass spectrometry, provides a nearly continuous palaeoceanographic record of the northeastern South China Sea for the last 15 000 yr. Planktic foraminiferal assemblages indicate that winter sea-surface temperatures (SSTs) r
Many general circulation models (GCMs) predict that high latitude environments will experience substantial warming over the next 100 years, which will be particularly pronounced during the winter months. Precipitation is also expected to increase but there is uncertainty as to the amount and spatial