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In the late 1980s, some scientists concluded that it was drought (or climate more generally), not overgrazing, that controlled the number of livestock in the semi-arid tropical rangelands with a high degree of rainfall variability (Behnke et al. 1993; Ellis and Swift 1988; Homewood et al. 1987).
From a certain degree of rainfall and number of females onward, however, the positive effect of each of these variables was weakened, as in the fetus model.
Our model shows that from a certain group size and degree of rainfall (i.e., environmental seasonality) onward, the positive effect is diminished in the fetuses of middle-ranking and even more so in those of low-ranking females.
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A calibrated distributed hydrologic model is employed to assess the relevance of these statistics in describing the degree of spatial rainfall organization, which is important for runoff modeling.
According to Hare (2003), CV is used to classify the degree of variability of rainfall events as less (CV < 20), moderate (20 < CV < 30), and high (CV > 30).
We used rainfall and NDVI data from GLEWS for the Ilmotiok (KOI-1) and Tiamamut (TIA-1) group ranches to determine the degree of correlation between rainfall at time t = 0 (days) and time t = 31 (days) where NDVI value = time t = 0 (days) in these two communities.
By averaging the elevation in 30-by-30 30-by-30 30-by-30 the scale from 1/120 degridsto 0.25 degree resolution, consistent weth the schanged rainfall dathe
Given the toll in lives and money, scientists like Dr. Staley and Dr. Kean are studying how and when slides happen — what characteristics of soil and underlying rock, what degree of slope and intensity of rainfall will cause a hillside to fail or a flood of mud to roar down a canyon, demolishing houses or whatever else is in its path.
Both series have been used to characterise the degree of convective contribution to rainfall, introducing the β parameter as the ratio between convective precipitation versus total precipitation in any period.
As many natural catchments exhibit a significant or even marked degree of seasonality in their rainfall and runoff data, the means of identification of the seasonality structure and the determination of a quantitative expression or index of seasonality are topics of considerable interest to hydrologists.
The degree of a tropical cyclone rainfall impact depends upon speed of movement, storm size, and degree of vertical wind shear.
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