Climate teleconnections influence on West Africa's terrestrial water storage-Reference-Cited by-同舟云学术

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Climate teleconnections influence on West Africa's terrestrial water storage

Published:2017-07-21 Issue:18 Volume:31 Page:3206-3224
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrol. Process.

Author:

Ndehedehe Christopher E.¹²^ORCID,Awange Joseph L.¹³,Kuhn Michael¹,Agutu Nathan O.¹⁴,Fukuda Yoichi³

Affiliation:

1. Department of Spatial Sciences; Curtin University; Perth Western Australia Australia

2. Department of Geoinformatics and Surveying; University of Uyo; Uyo Nigeria

3. Department of Geophysics; Kyoto University; Kyoto Japan

4. Department of Geomatic Engineering and Geospatial Information Systems; Jomo Kenyatta University of Agriculture and Technology; Nairobi Kenya

Funder

Curtin University-CSIRS

Publisher

Wiley

Subject

Water Science and Technology

Reference113 articles.

1. The version-2 Global Precipitation Climatology Project (GPCP) monthly precipitation analysis (1979Present);Adler;Journal of Hydrometeorology,2003

2. Assessing multi-satellite remote sensing, reanalysis, and land surface models' products in characterizing agricultural drought in East Africa;Agutu;Remote Sensing of Environment,2017

3. The use of GRACE data to monitor natural and anthropogenic induced variations in water availability across Africa;Ahmed;Earth Science Reviews,2014

4. Rotation of EOFs by the independent component analysis: Toward a solution of the mixing problem in the decomposition of geophysical time series;Aires;Journal of the Atmospheric Sciences,2002

5. The Sahelian standardized rainfall index revisited;Ali;International Journal Of Climatology,2009

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2. Understanding the shift in drivers of terrestrial water storage decline in the central Inner Mongolian steppe over the past two decades;Journal of Hydrology;2024-06

3. Impact of climate teleconnections on hydrological drought in the Sahel Region of Nigeria (SRN);Meteorology and Atmospheric Physics;2024-04-05

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