Showing posts with label Rain. Show all posts
Showing posts with label Rain. Show all posts

At times raindrops are bigger when it just begins to rain and sometimes smaller? What is the reason?



Rain happens when warm, moist air rapidly cools at high altitudes in the presence of surrounding colder air. At any given temperature, dry air can accommodate only a certain amount of water vapour. As the moist air temperature drops, due to cooling, it becomes super-saturated with water vapour. When air can accommodate no more water vapour under equilibrium conditions, it is saturated. Under super-saturated conditions, air holds more moisture than it possibly can under equilibrium conditions. Hence, there is the tendency of air to precipitate out any excess moisture present and it rains. Rain drops form due to condensation of water vapour around preferential sites such as microscopic dust particles, pollen grains etc. that are present in air. As the drop-wise condensation proceeds, microscopic droplets of water initially formed grow in size and the water droplet begins to fall under the action of gravity. While falling, the droplets can collide with other droplets and coalesce to form bigger droplets. Alternatively, droplets can collide with other droplets and break apart into smaller droplets due to the impact. There is another reason for the break-up of water drops. Due to the relative velocity between the falling water drop and the air around it, viscous shearing forces develop on the surface of the drop. These drag forces cause the drop to distort in shape. During its fall the waterdrop accelerates, and the magnitude of the drag forces increases roughly in proportion to the square of the fall speed of the drop. Due to shape distortions and the rapidly increasing effects of the shear stresses on the air-water interface of the drop, the drop may break apart. Large drops of water have a tendency to break apart more than the smaller ones. Due to these reasons growth of drop size due to coalescence, and break up due to collisions and viscous shear rain drops come in varying sizes, from the smallest to the largest, by the time they hit the ground.

Source: thehindu.com

Thunder is not always preceded by lightning but lightning is always followed by thunder. Why?




Thunder is always generated only by a lightning bolt. The bolt, 1 to 5 cm in diameter, could cause the air temperature to rise up to 30,000 degrees C (Compare it with Sun's surface (Photosphere) temperature of 5,400 degrees C). Such a sudden rise of air temperature causes explosive expansion of the bolt area to produce compression (or shock) waves that are heard as thunder or thunder rumblings.

The time lapse between the two in seconds multiplied by 330 gives roughly the distance of the lightning in metres.When there is a series of thunderclouds and the most rear one some 20 to 30 km away produces a lightning, the thunder may not be heard; especially so when the prevailing surface wind is towards the thundercloud.

Also, during a bright day, an isolated thundercloud may produce a lightning that can hardly be seen; but the thunder could be heard. Also, in a maturing thunder cloud with updrafts of 100 kmph or more, a lightning in the middle area of the cloud could be seen as a bright flash illuminating the upper portions of the cloud; the thunder may not be heard as the updrafts will disperse the sound waves. (A MIG jet aircraft approaching overhead can be seen but the sound can be heard only after it passes over your head).

When thunderclouds merge as in the `eye wall' of a very severe cyclone wherein the sustained surface wind speed exceeds 150 kmph, rapid collision of positively charged areas with negatively charged areas could produce intermittent flashes of lightning without producing thunder. This, I have personally observed for hours from very close quarters to the `eye wall'. This was confirmed under similar situations by some highly experienced meteorologists by independent judgement.

Source: thehindu.com