by neufer » Wed Sep 05, 2012 4:20 pm
Stephen Rasey wrote:
“The most powerful storm to affect the Bering Sea coast of Alaska in 37 years is pounding Alaska’s west coast and Eastern Siberia with hurricane-force winds, a destructive storm surge up to 7 feet high, waves up to 35 feet high, and blinding snow,” ...." central pressure of 945 mb." ... "6 foot storm surge in Nome Alaska." -- November 8-9, 2011.
That sounds like a "hurricane" to me. A polar cyclone, but a hurricane by another name.
Should storms like these be on the map?
Tropical cyclones are (condensation warmed) warm core circulations whose strongest winds are in the near surface boundary layer.
Polar cyclones are (radiation cooled) cold core circulations whose strongest winds are in the middle (or upper) atmosphere.
http://en.wikipedia.org/wiki/Polar_cyclone wrote:
<<A polar vortex (also known as Polar cyclones, polar vortices, Arctic cyclones, sub-polar cyclones, and the circumpolar whirl) is a persistent, large-scale cyclone located near one or both of a planet's geographical poles. On Earth, the polar vortices are located in the middle and upper troposphere and the stratosphere. They surround the polar highs and lie in the wake of the polar front. These cold-core low-pressure areas strengthen in the winter and weaken in the summer.
They usually span 1,000–2,000 kilometers in which the air is circulating in a counter-clockwise fashion (in the northern hemisphere). The reason for the rotation is the same as any other cyclone, the Coriolis effect.
Other astronomical bodies are also known to have polar vortices, including Venus (double vortex - that is, two polar vortices at a pole ), Mars, Jupiter, Saturn and Saturn's moon Titan.>>
http://en.wikipedia.org/wiki/Tropical_cyclone wrote:
<<A tropical cyclone is a storm system characterized by a low-pressure center and numerous thunderstorms that produce strong winds and heavy rain.
They usually span 300–700 kilometers. Tropical cyclones strengthen when water evaporated from the ocean is released as the saturated air rises, resulting in condensation of water vapor contained in the moist air. They are fueled by a different heat mechanism than other cyclonic windstorms such as nor'easters, European windstorms, and polar lows.
The characteristic that separates tropical cyclones from other cyclonic systems is that at any height in the atmosphere, the center of a tropical cyclone will be warmer than its surroundings; a phenomenon called "warm core" storm systems. A tropical cyclone's primary energy source is the release of the heat of condensation from water vapor condensing, with solar heating being the initial source for evaporation. Therefore, a tropical cyclone can be visualized as a giant vertical heat engine supported by mechanics driven by physical forces such as the rotation and gravity of the Earth. In another way, tropical cyclones could be viewed as a special type of mesoscale convective complex, which continues to develop over a vast source of relative warmth and moisture. While an initial warm core system, such as an organized thunderstorm complex, is necessary for the formation of a tropical cyclone, a large flux of energy is needed to lower atmospheric pressure more than a few millibars (0.10 inch of mercury). The inflow of warmth and moisture from the underlying ocean surface is critical for tropical cyclone strengthening. A significant amount of the inflow in the cyclone is in the lowest 1 kilometre of the atmosphere.>>
[quote="Stephen Rasey"]
[quote]“The most powerful storm to affect the Bering Sea coast of Alaska in 37 years is pounding Alaska’s west coast and Eastern Siberia with hurricane-force winds, a destructive storm surge up to 7 feet high, waves up to 35 feet high, and blinding snow,” ...." central pressure of 945 mb." ... "6 foot storm surge in Nome Alaska." -- November 8-9, 2011. [/quote]
That sounds like a "hurricane" to me. A polar cyclone, but a hurricane by another name.
Should storms like these be on the map?[/quote]
[list][size=200]No![/size][/list]
[b][color=#FF0000]Tropical cyclones are (condensation warmed) [u]warm core[/u] circulations whose strongest winds are in the near surface boundary layer.[/color]
[color=#0000FF]Polar cyclones are (radiation cooled) [u]cold core[/u] circulations whose strongest winds are in the middle (or upper) atmosphere.[/color][/b]
[quote=" http://en.wikipedia.org/wiki/Polar_cyclone"]
[float=right][img3="[b][color=#0000FF]Hubble view of the colossal [u]cold core[/u] polar cloud on Mars[/color][/b]"]http://upload.wikimedia.org/wikipedia/commons/d/de/Mars_cyclone.jpg[/img3][/float]
<<A polar vortex (also known as Polar cyclones, polar vortices, Arctic cyclones, sub-polar cyclones, and the circumpolar whirl) is a persistent, large-scale cyclone located near one or both of a planet's geographical poles. On Earth, the polar vortices are located in the middle and upper troposphere and the stratosphere. They surround the polar highs and lie in the wake of the polar front. These cold-core low-pressure areas strengthen in the winter and weaken in the summer. [b][color=#0000FF]They usually span 1,000–2,000 kilometers[/color][/b] in which the air is circulating in a counter-clockwise fashion (in the northern hemisphere). The reason for the rotation is the same as any other cyclone, the Coriolis effect.
Other astronomical bodies are also known to have polar vortices, including Venus (double vortex - that is, two polar vortices at a pole ), Mars, Jupiter, Saturn and Saturn's moon Titan.>>[/quote][quote=" http://en.wikipedia.org/wiki/Tropical_cyclone"]
[float=right][img3="[b][color=#FF0000]Tropical cyclones are (condensation warmed) [u]warm core[/u] circulations
whose strongest winds are in the near surface boundary layer.[/color][/b]"]http://upload.wikimedia.org/wikipedia/commons/thumb/f/fb/Hurricane_profile.svg/500px-Hurricane_profile.svg.png[/img3][/float]
<<A tropical cyclone is a storm system characterized by a low-pressure center and numerous thunderstorms that produce strong winds and heavy rain. [b][color=#FF0000]They usually span 300–700 kilometers.[/color][/b] Tropical cyclones strengthen when water evaporated from the ocean is released as the saturated air rises, resulting in condensation of water vapor contained in the moist air. They are fueled by a different heat mechanism than other cyclonic windstorms such as nor'easters, European windstorms, and polar lows. [b][color=#FF0000]The characteristic that separates tropical cyclones from other cyclonic systems is that at any height in the atmosphere, the center of a tropical cyclone will be warmer than its surroundings; a phenomenon called "[u]warm core[/u]" storm systems.[/color][/b] A tropical cyclone's primary energy source is the release of the heat of condensation from water vapor condensing, with solar heating being the initial source for evaporation. Therefore, a tropical cyclone can be visualized as a giant vertical heat engine supported by mechanics driven by physical forces such as the rotation and gravity of the Earth. In another way, tropical cyclones could be viewed as a special type of mesoscale convective complex, which continues to develop over a vast source of relative warmth and moisture. While an initial warm core system, such as an organized thunderstorm complex, is necessary for the formation of a tropical cyclone, a large flux of energy is needed to lower atmospheric pressure more than a few millibars (0.10 inch of mercury). The inflow of warmth and moisture from the underlying ocean surface is critical for tropical cyclone strengthening. A significant amount of the inflow in the cyclone is in the lowest 1 kilometre of the atmosphere.>>[/quote]