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The Coastal Waters of Southeast Alaska and British Columbia is a marine area designated by the International Hydrographic Organization (IHO).. It comprises waterbodies along the Pacific coast of British Columbia, Canada, and the Alaska Panhandle, United States; some waters off north-west Washington are also included.
Ketchikan, Alaska seen from Tongass Narrows in August 2009. Tongass Narrows is a Y-shaped channel, part of Southeast Alaska's Inside Passage.The waterway forms part of the Alaska Marine Highway and as such, is used by charter, commercial fishing, and recreational vessels, as well as commercial freight barges and tanks, kayaks and passenger ferries.
Alaska's portion of the Inside Passage extends 500 miles (800 km) from north to south and 100 miles (160 km) from east to west. The area encompasses 1,000 islands and thousands of coves and bays. While the Alexander Archipelago in Alaska provides some protection from the Pacific Ocean weather, much of the area experiences strong semi- diurnal ...
The forecast begins by listing areas with gale warnings, followed by a general synopsis of pressure areas, then a forecast for each individual sea area covering wind speed and direction, precipitation, and visibility. Extended forecasts at 00:48 and 05:20 include information from coastal weather stations and an inshore waters forecast.
Marine weather forecasting is the process by which mariners and meteorological organizations attempt to forecast future weather conditions over the Earth's oceans. Mariners have had rules of thumb regarding the navigation around tropical cyclones for many years, dividing a storm into halves and sailing through the normally weaker and more ...
Lynn Canal's location as a penetrating waterway into the interior connects Skagway and Haines, Alaska, to Juneau and the rest of the Inside Passage thus making it a major route for shipping, cruise ships, and ferries. During the Klondike Gold Rush it was a major route to the boom towns of Skagway and Dyea and thence to the Klondike gold fields.
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The mean transport of the baroclinic current near Kodiak Island in the western gulf of Alaska is approximately 10 Sv in the upper 1500 m. [4] The Alaska Current, together with the Gulf of Alaska, has an impact on the climate system of the southwestern United States, including seasonal rainfall and snow.