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Times of the Islands Winter 2018/19

Presents the "soul of the Turks & Caicos Islands" with in-depth features about local people, culture, history, environment, businesses, resorts, restaurants and activities.

Presents the "soul of the Turks & Caicos Islands" with in-depth features about local people, culture, history, environment, businesses, resorts, restaurants and activities.

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This image explains <strong>the</strong> concepts <strong>of</strong> sea breeze and cloud formation.<br />

erally blow from high pressure towards lower pressure,<br />

which during <strong>the</strong> day is from <strong>the</strong> ocean to <strong>the</strong> land. At<br />

night, we normally see <strong>the</strong> reverse situation—winds blowing<br />

from land out to sea.<br />

One final factor that will play into cloud formation<br />

has to do with <strong>the</strong> amount <strong>of</strong> moisture in <strong>the</strong> air. And<br />

we know based on geographic location that <strong>the</strong>re is an<br />

abundance <strong>of</strong> moisture in <strong>the</strong> atmosphere generally at all<br />

times over <strong>the</strong> <strong>Islands</strong>.<br />

Now let’s discuss <strong>the</strong> “hows” <strong>of</strong> cloud formation.<br />

Clouds are a conglomeration <strong>of</strong> trillions and trillions <strong>of</strong><br />

molecules <strong>of</strong> water vapor. Generally unseen to <strong>the</strong> naked<br />

eye, yet felt on <strong>the</strong> skin as humidity, water vapor once<br />

compacted into large areas reveals itself as clouds.<br />

How is it we see <strong>the</strong>se clouds? In <strong>the</strong> Caribbean, we<br />

can thank <strong>the</strong> salt in <strong>the</strong> ocean for this! In order to see<br />

clouds, we depend on what is called Cloud Condensation<br />

Nuclei, abbreviated as CCN. These are particles <strong>of</strong> dust,<br />

salt, pollution, and even sand from <strong>the</strong> Saharan Desert.<br />

Water vapor by nature, will need something to condense<br />

to in order for us to see it visibly. These CCN stick to<br />

water vapor, which is <strong>the</strong> single most important item we<br />

need for cloud formation. For <strong>the</strong> <strong>Islands</strong>, salt water evaporates<br />

<strong>of</strong>f <strong>the</strong> surface <strong>of</strong> <strong>the</strong> ocean and rises into <strong>the</strong> air<br />

as <strong>the</strong> CCN needed. However in order to see <strong>the</strong>se as<br />

clouds we need something else to occur.<br />

During <strong>the</strong> day, as <strong>the</strong> land heats up and low pressure<br />

develops over <strong>the</strong> land, <strong>the</strong> warm air rises in convective<br />

currents <strong>of</strong>f <strong>the</strong> hot ground into <strong>the</strong> air above <strong>the</strong> <strong>Islands</strong>.<br />

As <strong>the</strong> winds blow <strong>of</strong>f <strong>the</strong> water and arrive on land, <strong>the</strong>y<br />

get naturally deflected up as <strong>the</strong>y encounter topography<br />

and <strong>the</strong> much warmer air that is also rising. As this wind<br />

and air rises, it naturally begins to cool once again. And<br />

as that air cools, it also condenses. Those trillions <strong>of</strong><br />

molecules <strong>of</strong> water vapor become visible as tiny water<br />

droplets. And in mass, <strong>the</strong>y are visible as <strong>the</strong> fluffy white<br />

clouds we see across <strong>the</strong> <strong>Islands</strong>.<br />

If you would like to see this in action on a smaller<br />

scale, boil a pot <strong>of</strong> water on <strong>the</strong> stove. As <strong>the</strong> water boils,<br />

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<strong>Times</strong> <strong>of</strong> <strong>the</strong> <strong>Islands</strong> <strong>Winter</strong> <strong>2018</strong>/<strong>19</strong> 15

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