Tag Archives: Leeward

A Lesson in Meteorology: Windward and Leeward

There are two sides to a coin. Heads or Tails. One coin, two different sides. Now shift your thoughts from a coin to a mountain or an island. Perhaps even a mountainous island. Think of the coin. Think of the island. In meteorology, the study of earth’s atmosphere, there are two sides to any island—the windward side and the leeward side.

The Windward Side

This is the colder, wetter side of an island. It is subject to consistent winds that blow cool, moist air upward. As this air is lifted, due to a decrease in atmospheric pressure, it begins to cool (scientifically called adiabatic cooling). Cooler air is not able to hold as much water vapor as warm air, so at some point the moisture in the air begins to condense and clouds form. Rain.

The Leeward Side

As condensation occurs, it releases heat into the surrounding air. This effect is called latent heat of condensation. By the time the air descends down the other side of an island (or mountain), most of its moisture has been condensed out. As the air continues to descend towards sea level, atmospheric pressure increases which causes a temperature increase. Because of all of this (scientifically called adiabatic warming), the leeward side is generally warmer and drier.

Why Does This Matter?

Climate is a significant driving factor in the creation and sustainability of ecosystems and habitats. The prevalence of rain on windward sides of islands promotes the growth of vegetation whereas the leeward side flora is acclimated to a drier climate. Catalina island is no exception to this rule. The backside of Catalina, which faces open ocean is considered the windward side. The side that faces the mainland is the leeward. Studies are being done to better understand the effect that orographic effect has on micro-habitats. The iconic kelp forest, for one.

For more reading: https://www.climate.gov/

Image Sources: https://www.britannica.com/science/rain-shadow

 

Waves 101

Waves start far away from the beach, out in the open water. As wind brushes up along the ocean, friction is created between the wind and the water, transferring energy from the wind to the water molecules. As the wind continues to push against the water, it can force smaller wave energy together forming larger waves. When the wave energy reaches the coast, the water starts to run into the ocean floor and is slowed down by friction. The closer the water gets to shore, the more shallow it is, causing more water molecules to come in contact with the ocean floor and slow down. As the energy moves closer to shore, the surface water continues forward at the same speed while the deep water continues to slow down. Eventually the water at the surface crashes over itself forming waves we see on the beach.

Screen Shot 2015-06-09 at 7.45.24 PM

Photo Credit: http://www.geography.hunter.cuny.edu/~tbw/ncc/Notes/chap3.landforms/oceans
.coastal.processes.landforms/waves/wave.formation.breakers.htm

The size of the wave depends on many different factors. First which of is the speed of the wind, the faster the wind travels the bigger the wave will be. This is due to the greater force of which the wind places on the ripples of the ocean. The second factor is the fetch, or the amount of time wind is blowing over a certain area of water. Waves will continue to get larger the longer wind blows across the water.

Larger waves tend to be formed farther from shore than smaller waves which are created right offshore. Waves that start far offshore are typically called swell waves because they have much more time to build in the open water. Large storms have the perfect conditions for forming large waves due to the amount of wind and pressure that is pushing against the ocean.

Surfers monitor the weather conditions and patterns to determine if the surf will be large or small. Here on Catalina Island the best surf comes from the windward, or the open ocean side of the island. This is due to the open ocean swell that builds up over time reaching the island as large waves. On the leeward or the channel side of the island there are little to no waves. The island acts as a wind shadow, protecting the channel from wind and therefore preventing the formation of large waves. Here at CIMI we are on the leeward side of the island, which produces little to no waves. Can you figure out where we are surfing?

Waves 101

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We would like to thank you for visiting our blog. Catalina Island Marine Institute is a hands-on marine science program with an emphasis on ocean exploration. Our classes and activities are designed to inspire students toward future success in their academic and personal pursuits. This blog is intended to provide you with up-to-date news and information about our camp programs, as well as current science and ocean happenings. This blog has been created by our staff who have at least a Bachelors Degree usually in marine science or related subjects. We encourage you to also follow us on Facebook, Instagram, Google+, Twitter, and Vine to see even more of our interesting science and ocean information. Feel free to leave comments, questions, or share our blog with others. Please visit www.cimi.org for additional information. Happy Reading!

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