Owing to the low atmospheric humidity , insolation during the hours of sunshine is so intense that the ground becomes rapidly heated , often to temperatures of 70 C . The nocturnal radiation is also equally rapid , so that there is nightly chill or even frost , with the air temperature sinking below zero . निम्न वायुमंडलीय नमी के कारण जितनी देर धूप रहती है उतनी देर सूर्यातप इतना प्रचंड हो जाता है कि जमीन तेजी से गर्म हो जाती है और तापमान प्राय : 70 से . तक पहुंच जाता है.रात्रिकालीन विकिरण भी उसी तरह तेजी से होता है जिसकी वजह से रात को ठिठुरन हो जाती है या पाला तक पड़ जाता है तथा तापमान शून्य से नीचे चला जाता है .
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