Dry or humid? Mid-Holocene humidity changes in arid and semi-arid China
Spatial changes of effective moisture during the mid-Holocene have been reconstructed based on the compilation of recently published paleoclimate records, including ice core, lake level, pollen assemblage, and loess-paleosol records. Both geological data and the spatial pattern indicate that it was...
Main Authors: | , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2006
|
Subjects: | |
Online Access: | http://d-scholarship.pitt.edu/23362/ http://d-scholarship.pitt.edu/23362/1/licence.txt |
Summary: | Spatial changes of effective moisture during the mid-Holocene have been reconstructed based on the compilation of recently published paleoclimate records, including ice core, lake level, pollen assemblage, and loess-paleosol records. Both geological data and the spatial pattern indicate that it was dry in deserts during the mid-Holocene, but the timing of the beginning and end of dry intervals differs from place to place. Deserts having higher aridity index values remain dry longer. Dry intervals during the mid-Holocene are more possibly asynchronous than synchronous in arid and semi-arid China. In the Xinjiang region, except in sites located in deserts, the climate is generally wet during 7000-5000 a BP. In the northern Qinghai-Tibetan Plateau, effective moisture in most sites began to decrease after 5000 a BP. The climate became dry after 4000 a BP except in the deserts in the Loess Plateau and the Inner Mongolia Plateau. © 2005 Elsevier Ltd. All rights reserved. |
---|