Surface winds in some Alaskan passes

by G. Philip Weber

Publisher: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories in Seattle, Wash

Written in English
Published: Pages: 16 Downloads: 508
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  • Winds -- Alaska

Edition Notes

StatementG. Philip Weber
SeriesNOAA technical memorandum ERL PMEL -- 51
ContributionsEnvironmental Research Laboratories (U.S.)
The Physical Object
Paginationvii, 16 p. :
Number of Pages16
ID Numbers
Open LibraryOL13607581M

There are two ways to get Windows A short quiz will help you decide whether to buy Windows 10 to install on your current PC, or to buy a new Windows 10 PC. Peru Current, cold-water current of the southeast Pacific Ocean, with a width of about km ( mi). Relatively slow and shallow, it transports only ,,–,, cu ft (10,,–20,, cu m) of water per second. It is an eastern boundary current similar to the California C. Upward transport of the cold surface air is then hindered by the stable conditions. If winds are low, a temperature inversion typically develops near the surface as shown in Figure If winds are strong, the cold surface air is forced upward by mechanical turbulence and moderately stable conditions extend to some depth in the atmosphere. Total snow accumulations 12 to 20 inches near White Pass. Lower snow accumulations of 2 to 4 inches near sea level before 6 AM Sunday. * WHERE Klondike Highway above feet.

Explanation of WAM. Use the Weather Access Map (W.A.M.) to get current weather conditions and point forecasts for established locations.; You may also drag the magnifying glass icon to any location on the map for the latest forecast. Current Weather in 2 formats. In the spring of , a dust devil passed right by the National Weather Service station at Albuquerque, New Mexico. The station's anemometer, a device that measures windspeed, measured the wind gusts at 70 mph ( kph). A cold, snowy wind similar to Russia's purga is Alaska's "burga" (pronounced BOOR-guh), also spelled "boorga.". Climate (–Present) Anchorage, Ted Stevens Anchorage International Airport (0 miles) Take a look at our website widgetsAvailable free! Find Out More. Strongest 18 August, mph NNE; Average –Present mph. Swells are typically smooth waves, not choppy like wind waves. A swell is measured from the crest (top) to the trough (bottom). Ocean Currents An ocean current is a continuous flow of water in the ocean. Some currents are surface currents while other currents are much deeper flowing hundreds of feet below the surface of the water.

  The Alaska Dispatch writes: “Rain, sometimes heavy, is forecast for Seward, Valdez and Cordova, with winds accelerating through mountain passes. . CHAPTER 5 • ATMOSPHERIC PRESSURE, WINDS, AND CIRCULATION PATTERNS above the mercury in the pan, leaving a vacuum bubble at the closed end of the tube (Fig. ).At this point, the pressure exerted by the atmosphere on the open pan of mercury was equal. Surface high pressure centers are pretty much just the opposite situation. Winds spin clockwise (counterclockwise in the southern hemisphere) and spiral outward (in both hemispheres). The outward motion is called divergence. Air sinks in the center of surface high pressure to replace the diverging air. The sinking air is compressed and warms. We are customizing your profile. Application. We are customizing your profile.

Surface winds in some Alaskan passes by G. Philip Weber Download PDF EPUB FB2

In her beautifully written memoir, “Winds of Skilak: A Tale of True Grit, True Love and Survival in the Alaskan Wilderness,” Bonnie invites us into a routine that began in when she was 25 and Sam, /5().

AWARD-WINNING FINALIST in the Autobiography/Memoir category of the USA Best Book Awards. Leaving behind friends, family, and life as they know it, Sam and Bonnie Ward embark on a journey into the Alaskan wilderness that will change them forever. Winds of Skilak traces a young couple’s adventurou/5.

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Everyday low prices and free delivery on eligible : G. Philip Weber. ALASKAN GLACIER WINDS 99 During midsummer ofwind observations were made on two glaciers in Alaska (Fig. 1) to examine the frequency and diurnal variation of glacier winds and the differences due to location and exposure.

THE WORTHINGTON GLACIER This glacier is located in the Chugach Range some 25 miles (40 km.) from. Winds: An Alaskan Legend [Marasli, Armen] on *FREE* shipping on qualifying offers.

Winds: An Alaskan Legend. US Dept of Commerce National Oceanic and Atmospheric Administration National Weather Service Alaska Aviation Weather Unit Sand Lake Road Anchorage, AK View hotel, car, and ride reservations.

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Solutions initialized well on position of the major features, but the surface analysis showed the low near Banks Island about 3 to 4 mb deeper, and the low north of Utqiagvik about 2 mb deeper which explains the surface winds along the coast being 5 to 10 mph stronger than the guidance.

Solutions have improved some in the midrange and the. Select any of the following topics to see some typical reasons for activation difficulty, along with possible ways to get going again. Missing product key or digital license Windows 10 activation requires either a character Windows product key or a Windows digital license.

Use multiple desktops in Windows 10 to organize projects, or quickly switch between desktops before a meeting. In some locations, strong winds dam up on the windward side of steep mountain ridges then sweep down the leeward side in fierce gusts known as "williwaws." In the northwest Sound fierce "katabatic" or "fall winds" can accelerate down glacier valleys blasting the ordinarily calm fiords.

evidence of orographic steering of winds in the coastal zone. Surface wind directions at Cherni Island, Thin Point, and Cold Bay often were attributable - 30% of the time at Cherni Island and Thin Point, 50% of the time at Cold Bay - to channeling wind by a gap in the Aleutian Range.

At Ugaiushak Island 30% of surface winds came from. Prevailing wind direction ( - ) Prevailing wind is the direction of highest precent frequency. Stations may have close secondary maximum owing to noticable differences from month to month.

The result of this turbulence is that the direction and speed of the wind at the higher levels (e.g., feet) tends to be transferred to the surface. Since the wind direction at the higher level is parallel to the isobars and its speed is greater than the surface wind, this transfer causes the surface wind to veer and increase in speed.

The sun set at p.m. Saturday in Fairbanks, Alaska, but the sky was still lit well after dark. A stunning display of the aurora borealis, or northern lights, brought dancing curtains of. 14 Things No One Tells You About Surviving An Alaska Winter. The legendary, brutal Alaskan winters scare away most of the tourists and the summer seasonal employees.

By November, those serious about Alaska are hunkering down for the winter and the snow is falling in earnest.

Surface winds are the winds that you feel outside near the surface of the Earth. This lesson looks into why winds exist in some locations and not others and also at the driving forces for these winds. What are the Winds. Wind can be defined as air currents or moving mass of air from high-pressure areas to low-pressure areas.

Typically, air under high pressure normally moves towards areas under low pressure. Thus, the greater the pressure difference, the faster the flow of air which creates moving air with a considerably strong force.

The NASA/JPL press release and a blog that Jeff Masters wrote contain some additional information. There is still ocean surface vector wind data from the European ASCAT system which provides a partial mitigation for QuikSCAT.

Ascending Pass. Descending Pass. Last modified on Ap PM US Dept. of Commerce |. Wind roses are graphical charts that characterize the speed and direction of winds at a location.

and made an estimation of hourly winds over some time period, typically 2 to 5 minutes in length. Atmospheric › Surface › Wind speed and direction. Dataset Highlights. Wind Roses by Month. This is web site is not supported on a 24x7 basis and should not be considered operational.

An avalanche (also called a snowslide) is an event that occurs when a cohesive slab of snow lying upon a weaker layer of snow fractures and slides down a steep slope. Avalanches are typically triggered in a starting zone from a mechanical failure in the snowpack (slab avalanche) when the forces of the snow exceed its strength but sometimes only with gradual widening (loose snow avalanche).

At the surface, aspects of wind-driven circulation cause the gyres (large anticyclonic current cells that spiral about a central point) to displace their centres westward, forming strong western boundary currents against the eastern coasts of the continents, such as the Gulf Stream–North Atlantic–Norway Current in the Atlantic Ocean and the Kuroshio–North Pacific Current in the Pacific.

About. Need help. Get a forecast by email. This map shows surface winds. When winds are high on the surface, takeoffs and landings may be turbulent.

Mont Ventoux (French: [mɔ̃ vɑ̃tu]; Provençal: Ventor) is a mountain in the Provence region of Southern France, located some 20 km (12 miles) northeast of Carpentras, the north side, the mountain borders the Drôme 1, m (6, ft), it is the highest mountain in the region and has been nicknamed the "Beast of Provence", the "Giant of Provence", or "The Bald.

NSSL Research: Damaging Winds. There are a variety of types of damaging winds formed by different thunderstorm processes, but thunderstorms produce some straight-line winds when the thunderstorm downdraft hits the ground and flows outward.

Anyone living in thunderstorm-prone areas of the world is at risk for experiencing this phenomenon. Alaskan Winds is a popular song by Alaska Alaska | Create your own TikTok videos with the Alaskan Winds song and explore 0 videos made by new and popular creators.

The Beginning - In the beginning God created the heavens and the earth. Now the earth was formless and empty, darkness was over the surface of the deep, and the Spirit of God was hovering over the waters. And God said, “Let there be light,” and there was light.

God saw that the light was good, and he separated the light from the darkness. God called the light “day,” and the darkness he. Compare the circular action of air in (Fig.

4) to the wind directions of the global winds shown in (Fig. Global winds are strong winds that always flow in the depicted pattern because of the earth's rotation. Within the region from the equator (0° latitudes) to 30° N and 30° S, these strong global wind currents are called the Westerlies.

What we do: NSSL's experimental Convection Allowing Models (CAMs) can predict maximum downdraft wind speeds every four hours out to 36 hours. BAMEX (Bow Echo and MCV Experiment) was a field experiment involving scientists from NSSL, NCAR, the NWS, and OU that was designed to gather data to understand bow echoes and their resulting high damaging surface winds.

Strong winds are predicted to push through large swaths of Alaska late Tuesday night and throughout Wednesday morning, reaching up to mph in some places in Southcentral and Interior Alaska.Download the Alaska Airlines mobile app for a touch-free travel experience.

Scan your boarding pass from 6 ft away, store your credit card, and more.Current wind map of Alaska, Greenland contains live wind speed and wind direction map showing prevailing winds in this area.

Also, a wind forecast map is available, the map includes all changes of wind for a 10 days period by 3 hours steps.