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Since geomorphic processes under arid, humid, glacial, and possibly other climate conditions can induce particular landforms, areas subject to periodic climate change often show polygenetic landform associations.
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Pedogenic processes are recognized even under arid climate where loessial soils display kaolinite depletion and more illitic IS phases than dust.
Near-surface physical and chemical process can strongly affect dissolved-ion concentrations and stable-isotope compositions of water in wetland settings, especially under arid climate conditions.
Precipitation is a critical factor triggering soil biogeochemical processes in arid and semi-arid regions.
This chapter discusses wind and water processes in arid regions.
Roughness significantly affects the hydrological and erosion processes in arid and semi-arid areas where biological soil crusts (biocrusts) are ubiquitous.
Stratigraphically it occurs between the Grabfeld and Weser formations, which formed under arid conditions.
The sediment deposition of stratum 5 supposedly proceeded under arid climatic conditions.
Surface water infiltration from ephemeral dryland streams is particularly important in hyporheic exchange and biogeochemical processes in arid and semi-arid regions.
Under arid climatic conditions, predominantly fluvial systems developed in the study area during SQ1 (An et al. 2011).
A rise in ECe following addition of high levels of organic wastes to soil suggests that with continued application, total soluble salts may reach toxic levels for some crops especially under arid and semi-arid conditions of Iran.
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