| Our Virtual Tours |
| All Local Listings |
| About Sheryl & Cathy |
| About Sequim |
| Home Finder |
| Area Maps |
| Info Links |
| Home Team Blog |
| Contact Us |
| Home |
|
About Sequim
Why does this happen? When warm marine air from the Pacific Ocean reaches the Olympics, it is forced upwards and cooled. The cold air can't hold as much moisture as warm air and it rains. But, it is the west side of the mountains that gets the drenching. That cold dry air then starts to flow down the eastern side of the range. As it descends, it warms itself by compression. This newly warmed air travels a considerable distance before it again becomes heavy with moisture, where it converges with other moisture laden air flowing inland from around the southern end of the Olympics. These bodies of precipitation usually converge off the lower end and eastern side of Puget Sound.
Sequim, because of its sheltered position close to the north end of the Olympics, is favored with dry air. The town gets a good flow of warmed mountain air, but before it has taken on much moisture. It is also under the influence of other air currents, which disperse clouds and prevent fog from forming. Only about three or four days of fog are expected annually. In addition, Sequim is almost completely protected from the onslaught of southwesterly storms that often blast the upper Puget Sound region. Rain maps and rainfall records, kept since the early part of the nineteenth century, indicate that one can expect an increase in rainfall of about 1.6 inches per mile as you travel west from Sequim, and an increase of about 1 inch traveling in the opposite direction. The "Blue Hole" extends about six miles west and seven miles east from Sequim, and from the Olympic foothills to the Strait of Juan de Fuca.
|
Address: 279 W Washington St |