Supplementary Material to: Desert dunes transformed by end-of-century changes in wind climate, by Andreas C.W. Baas & Lucie A. Delobel, Department of Geography, King’s College London, London, UK. Matlab matrices storing the analysis results of ensemble-mean DP, RDP, and RDDir, for the two time-periods over the entire HadGEM3-GC31-MM (N216) model grid. Each matrix is oriented in traditional map mode, with top-to-bottom rows spanning latitudes from +90° to -90° and left-to-right columns spanning longitudes from -180° to +180°.</p
The dynamics of a small linear dune on the northern margin of the Namib Sand Sea have been monitored...
Spring-summer winds from the south move moist air from the Gulf of Mexico to the Great Plains. Rainf...
This study explores validating and calibrating the wind regime predicted by Global Circulation Model...
Supplementary Material to: Desert dunes transformed by end-of-century changes in wind climate, by An...
Supplementary Material to: Desert dunes transformed by end-of-century changes in wind climate, by An...
Sand dunes in arid regions are conspicuous mobile landforms that require adaptation and mitigation s...
Erosion by wind is one of the most important factors in desert environment. Prevailing winds can shi...
Supplemental text describing methods for dune-field digitization, digitization sensitivity analysis,...
Aeolian sediments cover about 6% of the earth’s surface, of which 97% occur in arid regions, and the...
Dense vegetation bands aligned parallel to contour levels and alternating at regular intervals with ...
textThis dissertation combines studies of aeolian bedforms and aeolian dune-field patterns to create...
This repository contains the data used in: Gadal, C., Delorme, P., Narteau, C. et al. Local Wind ...
In the Great Eastern Sand sea mesures of wind have been realised, in february 1984, according to thr...
The dynamics of a small linear dune on the northern margin of the Namib Sand Sea have been monitored...
Sand Dune Geomorphology occurs much faster than most geological processes, and is heavily influenced...
The dynamics of a small linear dune on the northern margin of the Namib Sand Sea have been monitored...
Spring-summer winds from the south move moist air from the Gulf of Mexico to the Great Plains. Rainf...
This study explores validating and calibrating the wind regime predicted by Global Circulation Model...
Supplementary Material to: Desert dunes transformed by end-of-century changes in wind climate, by An...
Supplementary Material to: Desert dunes transformed by end-of-century changes in wind climate, by An...
Sand dunes in arid regions are conspicuous mobile landforms that require adaptation and mitigation s...
Erosion by wind is one of the most important factors in desert environment. Prevailing winds can shi...
Supplemental text describing methods for dune-field digitization, digitization sensitivity analysis,...
Aeolian sediments cover about 6% of the earth’s surface, of which 97% occur in arid regions, and the...
Dense vegetation bands aligned parallel to contour levels and alternating at regular intervals with ...
textThis dissertation combines studies of aeolian bedforms and aeolian dune-field patterns to create...
This repository contains the data used in: Gadal, C., Delorme, P., Narteau, C. et al. Local Wind ...
In the Great Eastern Sand sea mesures of wind have been realised, in february 1984, according to thr...
The dynamics of a small linear dune on the northern margin of the Namib Sand Sea have been monitored...
Sand Dune Geomorphology occurs much faster than most geological processes, and is heavily influenced...
The dynamics of a small linear dune on the northern margin of the Namib Sand Sea have been monitored...
Spring-summer winds from the south move moist air from the Gulf of Mexico to the Great Plains. Rainf...
This study explores validating and calibrating the wind regime predicted by Global Circulation Model...