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Last Updated: 12:28 AM GMT on November 15, 2009
— Last Comment: 11:16 PM GMT on November 14, 2009
| Posted by: Orcasystems, 11:33 PM GMT on November 08, 2009 |
Weather 456 Update:
532. Weather456 10:28 PM GMT on November 14, 2009 Hide this comment.
Quoting stormwatcherCI: Good evening, how are you feeling ? Heard you were sick .
I'm still a little shaken but not stirred. The blog looks so unfamiliar. ****************************************************************************************
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Since the pictures are refreshed very often during the day, if you check often, ensure you refresh your cache, or the picture when you load it. Hurricane Hunter Pictures can be updated as often as every 15 minute. I can see this TS BUSTED FORECAST ALIBI being very well used next season.. or even this one :)
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****************************************************************************************Tropical News of the Day Tropical Cyclones: Physics, Energetics and Mechanics
Posted by: Weather456,11:24 AM GMT on October 25, 2009
Today I will present an overview of the formation, development, maturity, decay of tropical cyclones using the power of physics, energetics and mechanics, and answer some of those not so obvious questions.
Why do we need warm sea surface temperatures?
A pre-existing disturbance is always needed to initiate development, whether it is a tropical wave, tropical low, surface trough, upper low, or sometimes a frontal boundary and extratropical cyclone. We often here that cyclones need warm sea surface temperatures but why? I mean water is water regardless of the temperature. The main reason why we need warm sea surface temperature lies in the fact that warm water is more energetic than colder waters. Tropical cyclones need warm moist air and the only source of such air is from the ocean. Temperature is simply the degree to which molecules move and evaporation can only occur if water molecules can escape the sea surface and enter the air and in order for that to occur; you need the temperature to be high.
How does a tropical cyclone cools the sea surface?
A tropical cyclone's winds causes upwelling of colder sub-surface waters but there is another process by which tropical cyclones remove heat from the ocean – evaporation. Evaporation is the process by which water molecules change from a liquid state (water) to a gaseous state (water vapour). Now the molecules in the liquid state are bonded closer than in the gaseous form and this pretty obvious if you ever boiled water. Now remember when I said warmer temperatures cause molecules to move faster, well to get those molecules spread out from the liquid form to the gaseous form you need energy (heat of evaporation). The heat comes from the surrounding ocean, which is referred to as latent heat. (more)
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Record storm surges hit Mid-Atlantic coast Posted by: JeffMasters,4:22 PM GMT on November 13, 2009
Record storm surges have caused major flooding along the North Carolina, Virginia, Maryland, and Delaware coasts over the past 24 hours, thanks to the powerful winds of a slow-moving Nor'easter energized by the remains of Hurricane Ida. Norfolk, Virginia, suffered its highest storm surge on record last night, when a surge of 5.96 feet hit the Sewells Point tide station. The previous record was 5.62' during Hurricane Isabel of 2003, with the Chesapeake-Atlantic Hurricane of 1933 close behind at 5.61'. Last night's peak surge did not hit at high tide, and the storm tide--the combination of surge plus the tide--peaked at 7.74' above Mean Lower Low Water (MLLW), slightly below the 7.89' storm tide of Hurricane Isabel.
........................ (read more)
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Updated: 12:28 AM GMT on November 15, 2009
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| Posted by: Orcasystems, 4:57 PM GMT on October 12, 2009 |
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View Comments (745)
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Updated: 11:30 PM GMT on November 08, 2009
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| Posted by: Orcasystems, 1:02 PM GMT on September 25, 2009 |
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Updated: 4:56 PM GMT on October 12, 2009
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Park Heights, Langford
Langford / Victoria, BC
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| Elevation: |
300 ft
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| Temperature: |
41.2 °F
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| Dew Point: |
34.9 °F
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| Humidity: |
78% |
| Wind: |
North
at
0.0 mph
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| Wind Gust: |
0.0 mph
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| Updated: 6:42 PM PST on November 14, 2009 |
| PWS Owner: IBCVICTO20 — Station History |
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Copyright © 2009 Weather Underground, Inc.
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