Exact(4)
Seeds of trees frequently have "wings" that permit wider distribution by wind.
First, a statistical analysis of the data was performed, including calculation of mean wind speeds, availability of data, annual and diurnal variations, the Weibull parameters and the distribution by wind direction.
As a result of its fine-grained abrasive character and widespread distribution by wind, volcanic ash is a major hazard to aviation while ash fallout to the ground can pose significant hazards to flora, fauna, and infrastructure (Casadevall 1994).
Poplar seed trichomes greatly facilitate the ability of seeds to float in the air and as a result, enhance their potential for long distance distribution by wind.
Similar(56)
Recent volcanic eruptions such as 2008 Chaitén, Chile (Martin et al.2009) and 2010 Eyjafjallajökull, Iceland (Ulfarsson and Unger2011) have reminded us that ash fall is one of the most hazardous volcanic products due to its widespread distribution by winds, and can pose far-field impacts to society.
Also we evaluate the performance of these flexible families relative to the widely-used Weibull distribution by using wind speed data measured in various regions of Turkey.
Pressure distributions created by wind flow on low slope roofs is an issue addressed by many wind tunnel studies and selective field experimental studies.
The feasibility of this combination was also suggested by the similar distributions of pollutant dispersion observed by wind roses and dispersion model.
Prominent mid-latitude jets are seen at cloud heights especially in the wind field derived from the temperature distribution by integrating the thermal wind equation assuming cyclostrophic balance (Newman et al, 1984).
Since the Venus atmosphere is considered to be in cyclostrophic balance, the meridional distribution of the zonal wind can be derived from the temperature distribution by integrating the thermal wind equation with an appropriate lower boundary condition (Newman et al., 1984).
When the distribution of wind potential by geographic regions is evaluated, wind speed is generally found to be 6.0 to 7.0 m/s on the Marmara, western Black Sea, and eastern Mediterranean coasts; 5.0 to 6.0 m/s on the western Mediterranean coasts; 7.0 to 8.5 m/s on the north western Aegean coasts; and 4.5 to 5.5 m/s in interior regions[9].
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