Landscape evolution and development of eolian-modified unconsolidated gravel surfaces and yardangs in the Hami Basin, China
Authors:
- Dehai ZhangDZDehai Zhang
- Guocan WangGWGuocan Wang
- Alex PullenAPAlex Pullen
- Jordan T. AbellJAJordan T. Abell
- Junliang JiJJJunliang Ji
- Tianyi ShenTSTianyi Shen
- 1 November 2020
- journal article
- research article
- Published by Elsevier in Geomorphology
- Vol. 368
Abstract
No abstract availableKeywords
Funding Information
- China Geological Survey, Ministry of Natural Resources
- National Natural Science Foundation of China
This publication has 57 references indexed in Scilit:
- Wind as the primary driver of erosion in the Qaidam Basin, ChinaEarth and Planetary Science Letters, 2013
- Wind erosion in the Qaidam basin, central Asia: Implications for tectonics, paleoclimate, and the source of the Loess PlateauGSA Today, 2011
- Global connections between aeolian dust, climate and ocean biogeochemistry at the present day and at the last glacial maximumEarth-Science Reviews, 2010
- Saharan dust storms and indirect aerosol effects on clouds: CRYSTAL‐FACE resultsGeophysical Research Letters, 2003
- Spatial and temporal characteristics of dust storms in China and its surrounding regions, 1960–1999: Relations to source area and climateJournal of Geophysical Research: Atmospheres, 2001
- Asian provenance of glacial dust (stage 2) in the Greenland Ice Sheet Project 2 Ice Core, Summit, GreenlandJournal of Geophysical Research: Oceans, 1997
- The paleoclimatic record provided by eolian deposition in the deep sea: The geologic history of windReviews of Geophysics, 1994
- The statistics of counting clasts in rudites: a review, with examples from the upper Palaeogene of southern California, USASedimentology, 1993
- Late Pleistocene Continental Climate and Oceanic Variability Recorded in Northwest Pacific SedimentsPaleoceanography and Paleoclimatology, 1991
- Glacial‐interglacial CO2 change: The Iron HypothesisPaleoceanography and Paleoclimatology, 1990