09.09.2019 Views

Times of the Islands Fall 2019

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.

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

Humidity is a function <strong>of</strong> <strong>the</strong> air temperature and <strong>the</strong><br />

dew point. “Relative humidity” is basically how close <strong>the</strong><br />

air is to 100% saturation. When we have 100% saturation<br />

<strong>of</strong> <strong>the</strong> air, <strong>the</strong> temperature and dew point are <strong>the</strong> same.<br />

Any time <strong>the</strong> dew point is less than <strong>the</strong> temperature, you<br />

will see relative humidity values be lower as well.<br />

Confused yet? Let’s talk a bit more about this dew<br />

point temperature. The dew point relates to how much<br />

water vapor is actually in <strong>the</strong> air. Water vapor is <strong>the</strong> gaseous<br />

form <strong>of</strong> water. As <strong>the</strong> dew point rises, so does <strong>the</strong><br />

amount <strong>of</strong> water vapor in <strong>the</strong> air. As dew points decrease,<br />

<strong>the</strong> amount <strong>of</strong> water vapor in <strong>the</strong> air also decreases.<br />

To understand this from a comfort perspective, we<br />

can look at this function in different climates. In <strong>the</strong><br />

<strong>Islands</strong>, wind flow is always from <strong>the</strong> water, which transports<br />

moisture over <strong>the</strong> <strong>Islands</strong>, contributing to higher<br />

dew point temperatures. Contrast <strong>the</strong> Caribbean climate<br />

against <strong>the</strong> climate <strong>of</strong> western New Mexico and o<strong>the</strong>r high<br />

desert areas.<br />

In Caribbean climates, it is routine to see dew point<br />

temperatures <strong>of</strong> 74º to 82ºF, while air temperatures<br />

hover around 88ºF. As mentioned earlier, travelers will<br />

note upon arrival to TCI that <strong>the</strong> air feels sultry, and to a<br />

degree, wet. Doing activities outside in a Caribbean climate<br />

has a marked effect on <strong>the</strong> body as well. As you<br />

begin to sweat, <strong>the</strong> ability <strong>of</strong> your body to cool itself<br />

is degraded. In order for you to perspire properly and<br />

maintain comfort, it is imperative that your body is able<br />

to get rid <strong>of</strong> heat via perspiration effectively. When <strong>the</strong><br />

air is already highly saturated, your body struggles to<br />

This lizard has <strong>the</strong> right idea for keeping cool.<br />

evaporate and add your perspiration to <strong>the</strong> already moist<br />

environment.<br />

This chart pairs dew point temperatures with comfort level. In Caribbean climates, it is routine to see<br />

dew point temperatures between 74º and 82ºF.<br />

Contrast that with western New Mexico where <strong>the</strong><br />

air temperature may be 93ºF and <strong>the</strong> dew point might<br />

be closer to 30º or 35ºF. Here, <strong>the</strong> air is very dry with<br />

lower amounts <strong>of</strong> water vapor. Just stepping outside in<br />

temperatures in <strong>the</strong> low 90s<br />

is usually still surprisingly<br />

comfortable. Start hiking and<br />

biking, doing any outdoor<br />

activity in this environment,<br />

and again your body will start<br />

to perspire to cool itself down.<br />

But <strong>the</strong>re is a big difference.<br />

Remember that <strong>the</strong> lower <strong>the</strong><br />

dew point, <strong>the</strong> less water vapor<br />

<strong>the</strong>re is in <strong>the</strong> air. As a result,<br />

<strong>the</strong> relatively dry air can efficiently<br />

evaporate sweat from<br />

your body. As this occurs, it<br />

is cooling your body by absorbing<br />

<strong>the</strong> heat via <strong>the</strong> process <strong>of</strong><br />

evaporation. Therefore, when<br />

comparing climates, <strong>the</strong>re are<br />

drastic differences in what <strong>the</strong><br />

MARTA MORTON—WWW.HARBOURCLUBVILLAS.COM<br />

18 www.timespub.tc

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!