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Experimental Evidence of Plant Thermoregulation and Its Implications for Climate Stability
DOI:
https://doi.org/10.30564/jasr.v8i4.12145Abstract
Ongoing experiments reveal that plants of different species actively regulate their surface temperature by means of varying their rate of evapotranspiration. The overall cooling under hot weather conditions and bright sunlight may amount to as much as 20 ℃. That degree of cooling is vital in order to counteract the relatively low albedo of the leaves and to leave the plant surface cooler than the ambient temperature. In colder, cloudy conditions, plants reduce their evapotranspiration, with resulting surface temperatures that may exceed ambient temperatures. The evolution of angiosperm forests, on account of their vascularised leaves and relatively high rate of transpiration, may have been a major factor in the cooling of the planet from 100 million years ago, when average global surface temperatures were 6 ℃ higher than today. In addition, a high rate of evapotranspiration will have triggered the inflow of humid air from the ocean, thereby enabling the flourishing of the forests across continents. Physical experiments carried out by the author indicate that water vapour condensation results in partial pressure changes, with resulting airflow, consequently, as physics dictates, cloud condensation over forests will give rise inevitably to ocean-to-continent airflow. Given the role of the forest-derived biotic pump in generating flying rivers over the Amazon Basin, deforestation can result in hydrological collapse. The regeneration and recovery of forests can help cool the Earth’s surface by at least 1 ℃ globally.
Keywords:
Thermoregulation; Biotic Pump; Hydrological Cycle; Global-Warming; Angiosperm Evapotranspiration; Global-CoolingReferences
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Peter Paul Bunyard