Late Holocene Landscape Collapse of a Trans‐Himalayan Dryland: Human Impact and Aridification-Reference-Cited by-同舟云学术

Late Holocene Landscape Collapse of a Trans‐Himalayan Dryland: Human Impact and Aridification

Published:2019-12-10 Issue:23 Volume:46 Page:13814-13824
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Menges Johanna¹^ORCID,Hovius Niels¹²^ORCID,Andermann Christoff¹^ORCID,Dietze Michael¹^ORCID,Swoboda Charlie²,Cook Kristen L.¹,Adhikari Basanta R.³,Vieth‐Hillebrand Andrea⁴^ORCID,Bonnet Stephane⁵^ORCID,Reimann Tony⁶,Koutsodendris Andreas⁷^ORCID,Sachse Dirk¹^ORCID

Affiliation:

1. Section 4.6GFZ German Research Centre for Geosciences Potsdam Germany

2. Institute of GeosciencesUniversity of Potsdam Potsdam‐Golm Germany

3. Department of Civil Engineering, Institute of EngineeringTribhuvan University Kirtipur Nepal

4. Section 3.2GFZ German Research Centre for Geosciences Potsdam Germany

5. GET CNRS Univ Toulouse, UMR 5563, 14, Avenue Édouard Belin Toulouse France

6. Soil Geography and Landscape group & Netherlands Centre for Luminescence datingWageningen University Wageningen The Netherlands

7. Institute of Earth SciencesHeidelberg University Heidelberg Germany

Funder

H2020 European Research Council

Horizon 2020 Framework Programme

Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GL084192

Reference86 articles.

1. Facies analysis and basin architecture of the Thakkhola‐Mustang Graben (Neogene‐Quaternary), central Nepal Himalaya;Adhikari B. R.;Austrian Journal of Earth Science,2011

2. Death and Burial among Two Ancient High-Altitude Communities of Nepal

3. Investigations into the potential effects of pedoturbation on luminescence dating

4. Toward a complete Himalayan hydrological budget: Spatiotemporal distribution of snowmelt and rainfall and their impact on river discharge

5. The Holocene Indian monsoon variability over the southern Tibetan Plateau and its teleconnections

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