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The building was considered in three Australian climate zones (zones 3, 5 and 7) representing hot arid, warm temperate and cool temperate climates, respectively.
The analysis was performed in three different climate zones in Australia, namely: climate zone 3, 5 and 7, representing hot arid, warm temperate and cool temperate climate, respectively.
The pedogenetic stages in subordinate landscapes of the forest-steppe and forest zones fall mainly into arid warm and, sometimes, humid warm and arid cold climatic phases of the 2000-year-long 2000-year-long 2000-year-longv rhythm.
The system, originally developed in 1900, relates the climate to vegetation and identifies five major climate types: equatorial, arid, warm temperate, snow, and polar.
Traditionally, agaves are commercially cultivated primarily as a fiber source, often in arid, warm regions; some can tolerate temperatures of up to 65°C [ 61] and are therefore a good feedstock candidate for second-generation biofuels in an African context, where residues could potentially be further processed in small-scale operations for heat or electricity generation.
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In the semi-arid warm temperate South Africa, the Gamtoos estuary experiences a full salinity gradient maintained by irregular but relatively frequent freshwater pulses, whereas the Kromme estuary is euhaline throughout its extent and receives only occasional freshwater inputs when the storage reservoir six km upstream overtops.
The climate of the area is semi-arid warm-Mediterranean, with a mean annual precipitation of 220 mm (with 37%% of inter-annual variation and 76 to 215 % of monthly variation).
The Shaximiao sandstones were deposited under semi-arid and warm conditions (Wang and Wang 2010), and the δ18OSMOW value of −8 ‰ was assumed for early diagenetic formation water based on the results of Zhang et al. (2008).
This trial showed that precipitation can modulate the impact of cultural practices on grape and wine composition, and that lower irrigation amounts do not correspond to reduced wine quality even in the semi-arid and warm conditions of Central California.
BSCs occur on all continents on Earth, in warm arid and semi-arid habitats as well as in other climate zones such as alpine regions, where soil moisture is limiting and cover provided by higher plants is sparse (Belnap and Lange 2001).
These climate characteristics differ from those of the monsoon area, which are mainly displayed in cold-arid and warm-wet synchronization but also restricted by the atmospheric circulation at high latitudes.
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