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Moisture supply sufficient to sustain channeled surface flow is governed primarily by climate, which regulates precipitation, temperature, and evapotranspiration water loss caused by vegetation.
Moister BL under a higher SST condition (via increased surface moisture supply) results in an enhanced BL FT moisture contrast.
It resulted from the onset of more favorable conditions, namely warming, increase of moisture supply and reduction of volcanic activity.
The dynamics of moisture supply was the main controlling factor, while the temperature fluctuations were of secondary importance.
The PDSI is widely used in drought evaluation studies, which was developed by Palmer (1965) to measure the cumulative departure in atmospheric moisture supply and demand.
These are lands that have the soil quality, growing season and moisture supply needed for producing high yields of crops sustainably.
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Tropical storms thrive on energy and moisture supplied by warmer water.
Under such a situation, the annual tree rings vary in width as a direct reflection of the moisture supplied.
The most favorable conditions in terms of heat and moisture supplies continued during the Middle Holocene, resulting in formation of dark humus horizons.
In the winter the plant forms a non-carnivorous rosette of small, fleshy leaves that conserves energy while food and moisture supplies are low.
It is then important to monitor soil moisture and supply water based on the soil condition.
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