The temperature field in the lowest layers of the atmosphere Over Poona
DOI:
https://doi.org/10.54302/mausam.v28i4.2767Keywords:
temperature field, lowest layers, atmosphere Over PoonaAbstract
Temperatures at two levels (1.2 metres a. g.1. and 36-58 metres a.g.1.) for the two random years 1949 and 1957 are analysed. Unstable thermal stratification during day time due to turbulence and eddies changing over to stable thermal stratification due to nocturnal cooling of the air layers and consequent inversion has been described high-lighting their time of occurrence and month to month variation.
Temperature variations for the year 1949 at the two levels have also been subjected to harmonic analysis.
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