KOHLER ANDRAE STATE PARK | SHEBOYGAN, WISCONSIN | LAKESIDE CAMPING SERIES
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- เผยแพร่เมื่อ 6 ก.ย. 2024
- We drive down into Wisconsin to continue our tour of camping on the Great Lakes. This time, we stop at Kohler-Andrae, a large state park with sand dunes and marshes right on the shores of Lake Michigan.
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Beautiful spot and who doesn’t like saying SHE BOY GAN??
I know, right??
Found this answer from James Marshall.....leave it to a Science Teacher:
James Marshall, Science Teacher
Waves don't always flow towards the shore, it just appears that way.
Sea waves are mostly formed by winds moving across the surface of the sea water, pushing the surface water along until it forms waves of energy. Winds form whenever there are parcels of high pressure air near areas of low pressure, and the high pressure air moves towards the area of low pressure in order to equalise the two air pressures. One type of wind is a sea breeze, caused by air over land warming faster than the air over nearby water. The warm air expands and rises, causing lower air pressure. Cooler air above the sea flows onto the land to replace the rising air on the land - a cooling sea breeze. The opposite occurs when the air on land cools faster than air over the sea, creating a land breeze. One type of breeze is moving towards the shore, the other moves off shore. One will push waves towards shore, the other will push waves away from shore. Waves can also be caused by storms or movement of land during an earthquake.
Out at sea there is a chaos of waves moving in multiple directions that were formed at various locations at sea and from various locations near land. Out at sea you can see waves randomly crashing into each other from different directions, creating white caps. Occasionally wave energies align with other wave energies and strengthen, causing rouge waves. Ship captains know that rouge waves can strike from any direction.
Most waves in deep water are water are barely noticeable as they move through the water. If they are travelling away from shore or parallel to shore, they remain in deep water. For the waves that are moving in the direction of a shoreline, the gradual shallowing of the water as you approach land causes the top of the wave to begin to move faster than the water underneath, which is restricted by friction. Eventually, the top of the wave rolls over, causing the wave to ‘break’. This action makes the wave very visible, so you easily notice it. Diffraction causes waves to spread out in all directions after a wave passes through a narrow gap, such as in a bay. Waves moving in to shore have had a long time to build up and are generally formed by a steadily blowing wind that moves in one direction, so are dominant. Waves moving in directions other than towards shore will generally not break and mostly go unnoticed. Waves moving away from shore during offshore breezes are only just beginning their journey, so are relatively minor.
Thanks, Doug!!
Thanks Doug!!!
Nice review 👌
Thank you!
Can you share what camp site you had? It looks perfect!
Sure! We were in site 88, which was an electric site. It was very private, yet close to everything.. I would recommend it!
What kind of parents are we? Don’t have a clue what our daughter is doing!
Poor Chompers!