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properties of weather radar returns have been analyzed to differentiate between hail and heavy rain.
The only case in which we can discuss multiple trajectories is in a multicellular thunderstorm where the hailstone may be ejected from the top of the "mother" cell and captured in the updraft of a more intense "daughter cell".

A cold front can push the marine layer coast-ward, an occurrence most typical in the spring or late fall.

It is essentially a radiation fog confined by local topography, and can last for several days in calm conditions.
Accordingly, hail is actually less common in the tropics despite a much higher frequency of thunderstorms than in the mid-latitudes because the atmosphere over the tropics tends to be warmer over a much greater depth. [24][25] The use of differential reflectivity (Zdr), in combination with horizontal reflectivity (Zh) has led to a variety of hail classification algorithms. In the case of dew, liquid forms because water droplets merge more readily on solid surfaces.

(UK, dialect) Tall and decaying grass left standing after the cutting or grazing season; foggage. See Cloud. When temperatures are low enough, dew takes the form of ice; this form is called frost.

The size of hail stones is best determined by measuring their diameter with a ruler.

A new growth of grass appearing on a field that has been mowed or grazed. Cloud Formation Processes", "Fog And Stratus – Meteorological Physical Background", Applying Fog Forecasting Techniques using AWIPS and the Internet, Climate education update: News and information about climate change for teachers and students, "Pogonip - Definition from the Dictionary.com". It has to be kept in mind that some of these methods include guttation, while others only measure dewfall and/or distillation. This up and down motion was thought to be responsible for the successive layers of the hailstone. is working on effective, foil-based condensers for regions where rain or fog cannot cover water needs throughout the year. [22][23]

Typical dew nights are classically considered to be calm because the wind transports (nocturnally) warmer air from higher levels to the cold surface. Fog commonly produces precipitation in the form of drizzle or very light snow. Particularly foggy places include[citation needed] Hamilton, New Zealand and Grand Banks off the coast of Newfoundland (the meeting place of the cold Labrador Current from the north and the much warmer Gulf Stream from the south). Based on existing data (Beysens et al., 2006; Klemm et al., 2012; Muselli et al., 2006; Sharan et al., 2011), although we believe fog and dew to be potable after some treatment, we encourage trace metal analyses especially in samples collected from areas influenced by industrial activities or areas with fog and/or dew that exhibits very low pH, since acidic pH of these waters could extract and elevate trace metal concentrations to levels harmful to human health.

Such high population growth rates and development pressures coupled with the potential impacts of global climate change (decrease in rainfall) are projected to increase water stress to more than 66% of the global population by 2025 (Beysens, 2018). ; it measured 8 inches (20 cm) in diameter and 18.62 inches (47.3 cm) in circumference, weighing in at 1.93 pounds (0.88 kg). Their results have not been able to be verified. This process distinguishes dew from those hydrometeors (meteorological occurrences of water) which are formed directly in air cooling to its dew point (typically around condensation nuclei) such as fog or clouds.

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