405, please remember to sign off with your name when you post as well as comment.

Wednesday, April 6, 2011

Types of rainfall

Hi everyone! I'll be sharing with everyone about the different types of rainfall today. Some might wonder, rain is simply water droplets falling back onto earth, how different could it possibly get?! But yes, there're in fact 3 different types of rainfall, and I'll be explaining them to you in detail.


1. Convectional rainfall


This is the type of rainfall we get in Singapore :) As the name suggests, it is a result of convection of the wind patterns on earth. Warm air rises and cold air sinks in the convectional current due to density. The hot air and the rays from the Sun intensely heat the ground, and the warm ground warms the air immediately above it. This produces a bubble of warm air that begins to rise. This air cools as it rises in the atmosphere and eventually reaches a dew point temperature causing clouds to form. As these clouds accumulate, the water vapour that has condensed to form water droplets inside will be too heavy, and fall back to earth as rain. This rain is usually heavy and lasts for only a short period of time.


Here's a simple illustration to aid everyone:





2. Orographic rainfall


You can find this type of rainfall at some of the earth's great deserts :) The word "orographic" means that it is related to mountains. When moist, warm air from the sea evaporates, the air is forced up against mountain slopes at places with mountains. At the tip of the mountain top, air formed is cooled at dew point, before condensing to form water droplets, which ultimately fall back down as rainfall. At mountainous regions, air drops down over the high ground, gaining temperature and increasing the amount of water it can hold. That is why the flat regions below mountains hardly experience rain, and this area is known as rain shadow. This is a diagram to illustrate orographic rainfall:



3. Frontal rainfall




Frontal rainfall is caused when frontal systems form when warm and often tropical air meets cooler air. Stratiform precipitation falls out of nimbostratus clouds. Nimbostratus clouds are a formless cloud layer that is almost uniformly dark grey. Usually, nimbostratus is a sign of steady moderate to heavy precipitation. It looks something like this:

Scary, isn't it?! ):
Back to the point on warm and cool air. As hot air is lighter and less dense than cold air, it rises over it. As warm air is forced to rise further, condensation occurs at dew point, and over time rain droplets will accumulate, resulting in the scary looking cloud as seen above (because the water droplets block out sunlight from the Sun).


On the other hand, when heavier and denser cold air pushes beneath and lifts the warm air, a cold front occurs. This causes lowered pressure along the cold front and can cause the formation of showers and thunderstorms when enough moisture is present.

Alright, I hope that everyone has learnt a new thing or two through this new entry. Tata for now :)

Done by: Clarissa (7)


9 comments:

  1. Thanks for Orographic lifting part.
    :)

    ReplyDelete
  2. waoh,thanks 4 refreshing my horizon

    ReplyDelete
  3. do you have any other really helpful info on Singapore?

    ReplyDelete
  4. Good article. I definitely appreciate this website.
    Continue the good work!
    Feel free to visit my site www.ngjobwatch.blogspot.com

    ReplyDelete
  5. Hello

    Never heard: Top new 2017

    What you say is illogical and stupid
    What you call:
    Convectional rainfall
    Orographic rainfall
    Frontal rainfall
    - Positive charges is hydrogen (H + ions), it is held most in altitude because, it is the lightest, it supports the coldest

    - Negative charges is monoatomic oxygen known very electronegative (O-- ions), it holds under it because it is heavier than hydrogen and supports less the coldSee here:


    http://pdf.lu/Jy1K/ In two pages (drawings included)

    - Compression, the result of the opposition of two mechanical forces (those of the ascending and descending air currents) bringing these two layers together (H and O), all gas is compressible, they combine in a real explosive chemical reaction "the synthesis of water in the atmosphere" and everything is explained as if by magic
    (lightning, thunder and rain = a single operation), the condensation only comes after the formation of water

    - You know better than I that any cloud is formed of molecules of water which are themselves bipolar (side positive hydrogen and side oxygen negative),

    - Water vapor does not rise as such (H2O) in the gaseous state but is decomposed into free H2 and O

    - Is it not difficult for you to imagine a positive cloud and a negative cloud? (It's even stupid to think)

    ReplyDelete