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  1. #41
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    12zECMWF in 7 days


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    WHXX01 KWBC 091852
    CHGHUR
    TROPICAL CYCLONE GUIDANCE MESSAGE
    NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL
    1852 UTC THU SEP 9 2010

    DISCLAIMER...NUMERICAL MODELS ARE SUBJECT TO LARGE ERRORS.
    PLEASE REFER TO NHC OFFICIAL FORECASTS FOR TROPICAL CYCLONE
    AND SUBTROPICAL CYCLONE INFORMATION.

    ATLANTIC OBJECTIVE AIDS FOR

    DISTURBANCE INVEST (AL922010) 20100909 1800 UTC

    ...00 HRS... ...12 HRS... ...24 HRS. .. ...36 HRS...
    100909 1800 100910 0600 100910 1800 100911 0600

    LAT LON LAT LON LAT LON LAT LON
    BAMS 12.3N 61.0W 12.4N 61.6W 12.7N 62.5W 13.0N 63.6W
    BAMD 12.3N 61.0W 12.2N 62.2W 12.3N 64.0W 12.4N 65.9W
    BAMM 12.3N 61.0W 12.2N 61.7W 12.4N 62.9W 12.6N 64.3W
    LBAR 12.3N 61.0W 12.5N 61.9W 13.1N 63.3W 13.8N 65.1W
    SHIP 20KTS 27KTS 37KTS 49KTS
    DSHP 20KTS 27KTS 37KTS 49KTS

    ...48 HRS... ...72 HRS... ...96 HRS. .. ..120 HRS...
    100911 1800 100912 1800 100913 1800 100914 1800

    LAT LON LAT LON LAT LON LAT LON
    BAMS 13.4N 64.9W 14.3N 68.3W 15.1N 71.8W 16.6N 75.3W
    BAMD 12.4N 68.1W 12.4N 73.4W 11.9N 79.2W 10.9N 85.0W
    BAMM 12.8N 66.1W 13.2N 70.0W 13.7N 73.8W 14.7N 77.3W
    LBAR 14.7N 67.3W 16.3N 72.4W 17.7N 77.6W 19.0N 81.9W
    SHIP 62KTS 78KTS 87KTS 96KTS
    DSHP 62KTS 78KTS 87KTS 96KTS

    ...INITIAL CONDITIONS...
    LATCUR = 12.3N LONCUR = 61.0W DIRCUR = 280DEG SPDCUR = 6KT
    LATM12 = 12.1N LONM12 = 59.8W DIRM12 = 281DEG SPDM12 = 5KT
    LATM24 = 11.9N LONM24 = 58.7W
    WNDCUR = 20KT RMAXWD = 40NM WNDM12 = 20KT
    CENPRS = 1009MB OUTPRS = 1011MB OUTRAD = 90NM SDEPTH = S
    RD34NE = 0NM RD34SE = 0NM RD34SW = 0NM RD34NW = 0NM







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  6. #45
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    squintdance New Tropical Tidbit by Levi32 for Thursday 9/09

    "The ultimate judge of your swing is the flight of the ball." - Ben Hogan

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    ..... Do, or do not. There is no 'try.' .....


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    30%

    Return to Atlantic Graphical TWO 1. DISORGANIZED CLOUDINESS AND THUNDERSTORMS IN THE VICINITY OF THE WINDWARD ISLANDS ARE ASSOCIATED WITH A NEARLY STATIONARY AREA OF LOW PRESSURE. THE LOW SHOULD BEGIN TO DRIFT WESTWARD AND IT APPEARS THAT THE ENVIRONMENT IS BECOMING A LITTLE LESS FAVORABLE FOR DEVELOPMENT DURING THE NEXT DAY OR TWO. THERE IS A MEDIUM CHANCE...30 PERCENT...OF THIS SYSTEM BECOMING A TROPICAL CYCLONE DURING THE NEXT 48 HOURS.




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  15. #54
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    Rob Lightbown:

    Tropical Weather Discussion

    Issued: Friday, September 10, 2010 620 am EDT/520 am CDT
    Eastern Caribbean Disturbance (Invest 92-L):

    I am also monitoring an area of disturbed weather in the far eastern Caribbean associated with an area of low pressure located very near the island of Tobago. Satellite imagery in the past couple of hours have indicated that banding features are starting to form with some curvature in the building convection. This is a clear sign to me that a surface circulation may be forming. With that said, developing systems like this tend to go through several cycles of building and dissipating convection and it would not at all surprise me to see this convection die off later today only to build again tomorrow morning.
    Most of the model guidance develops this system down the road around Monday and Tuesday and holds off on significant intensification until it is west of Jamaica on Wednesday and Thursday. The exception to this is the GFS model which forecasts no development. This makes me want to be very conservative now in forecasting development as the GFS model was the first model to key in on Gaston not redeveloping.
    As for the other model guidance, the European model forecasts significant intensification in the western Caribbean around the middle part of next week with a track over the Yucatan Peninsula next Friday before tracking across the Bay of Campeche next weekend and into northern Mexico next Monday (September 20th).
    The Canadian model is much further north and forecasts little or no development in the eastern Caribbean and forecasts 92-L to track north-northwestward this weekend and starts to develop and intensify it early next week when it’s north of Puerto Rico. Eventually, the Canadian model forecasts this system to interact with Igor by the middle to later part of next week and 92-L is pushed west-southwest into the Bahamas early next weekend and into the Florida Straits in about 9 to 10 days from now. I am skeptical regarding this run of the Canadian model as it takes in account the idea that Igor makes it all the way to the US East Coast and also takes in account that this system tracks as far north as 27 North Latitude, which both at this point seems unlikely.
    So, at this point, I am leaning strongly towards the idea of little or no development this weekend into Monday and Tuesday of next week while it is in the eastern and central Caribbean. I think this system may wait to develop and intensify until it is west of Jamaica, which is expected on Wednesday; so from Wednesday and beyond, I think development and intensification will become much more likely. With that said, all interests in the central and western Caribbean, including Jamaica, the Cayman Islands, Belize and the Yucatan Peninsula should closely monitor this system.
    "The ultimate judge of your swing is the flight of the ball." - Ben Hogan

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    Jeff Masters:

    92L still a threat to develop; record SSTs continue in the tropical Atlantic
    Posted by: JeffMasters, 8:44 AM CDT on September 10, 2010
    A tropical disturbance (92L) over the Lesser Antilles Islands lost most of its heavy thunderstorms last night, due to an infusion of dry air. However, 92L has redeveloped a moderate amount of heavy thunderstorm activity this morning, and remains a threat to the Caribbean--though not as great a threat as it appeared yesterday. Satellite loops show that 92L's heavy thunderstorms are slowly growing in areal coverage, and are becoming more organized. St. Lucia reported sustained winds of 33 mph this morning in a heavy rain squall, and heavy rain showers and gusty winds can be expected throughout the southern Lesser Antilles Islands today. Martinique radar shows that heavy rains are now affecting that island, but there is no rotation to the radar echoes evident. Surface observations indicate that pressures continue to fall at a number of stations in the Lesser Antilles, but no surface circulation is evident in the wind reports. A strong flow of upper level easterly winds is creating a moderate 10 - 20 knots of wind shear on the south side of 92L. The waters are at near-record warmth, 30°C, and these warm waters extend to great depth. Water vapor satellite loops show a large area of dry air lies over the northern Caribbean, and this dry air could interfere with development over the next few days.

    Forecast for 92L
    The disturbance is moving westward at 5 mph, but steering currents favor a more west-northwest motion Saturday. Lower shear lies over the Central Caribbean, away from the coast of South America, so any northward component of motion will allow for more significant development. There is drier air to the north, but 92L is steadily moistening the atmosphere in the Caribbean, so dry air may not be a problem for it. Model support for development is less than it was yesterday. The GFS and NOGAPS models do not develop 92L. The HWRF, GFDL, and UKMET models predict development, with a track taking 92L into the Dominican Republic on Sunday as Tropical Storm Julia. These models predict the storm will continue west-northwest, affecting Haiti, Eastern Cuba, Jamaica, and the Southeast Bahamas early next week. The ECMWF model foresees a more southerly track, taking 92L into Mexico's Yucatan Peninsula seven days from now.

    Residents of the northern Lesser Antilles Islands and Puerto Rico should anticipate the possibility of heavy rains from 92L affecting their islands on Saturday and Sunday, though most of the action will probably stay south and west. The southern Dominican Republic should see heavy rains of 3 - 6 inches on Sunday and Monday from 92L, and Haiti, Jamaica, and eastern Cuba should anticipate similar rains on Monday and Tuesday. Should 92L make a direct hit on the Dominican Republic, it could destroy the storm, though. NHC is giving 92L a 40% chance of developing into a tropical depression by Sunday, which is a reasonable forecast. The first Air Force Hurricane Hunter mission into 92L is scheduled for Saturday morning, but there will be two research missions into the storm today that will give us valuable information on 92L's large scale environment and potential for development.


    Figure 1. Morning satellite image of 92L.

    Igor
    Tropical Depression Igor has survived a bout with high wind shear, and is now in an environment of moderate 10 - 20 knots of shear that should allow for steady strengthening. Waters are warm, 28°C, and the Saharan Air Layer (SAL) is probably not close enough to Igor to prevent development. The models continue to predict development of Igor into a hurricane 2 - 4 days from now. Igor will track west to west-northwest over the next week, with long range forecasts from the GFS and ECMWF models putting the storm several hundred miles northeast of the Lesser Antilles Islands about 6 - 8 days from now. Climatology shows that about 10% of all tropical cyclones that have existed at Igor's current position have gone on to hit the U.S. East Coast; these odds are about 5% for Canada. The forecast steering pattern for the coming two weeks from the GFS model shows a continuation of the pattern we've seen all hurricane season, with regular strong troughs of low pressure moving off the U.S. East Coast. This pattern favors Igor eventually recurving out to sea without affecting any land areas. The odds of Igor hitting land in the U.S. or Canada are probably close to their climatological 10% and 5% probabilities, respectively.

    Elsewhere in the tropics
    The GFS and ECMWF models predict the development of a new tropical wave off the coast of Africa 3 - 6 days from now.

    August SSTs in the tropical Atlantic set a new record
    Sea Surface Temperatures (SSTs) in the Atlantic's Main Development Region for hurricanes had their warmest August on record, according to an analysis I did of historical SST data from the UK Hadley Center. SST data goes back to 1850, though there is much missing data before 1910 and during WWI and WWII. SSTs in the Main Development Region (10°N to 20°N and 20°W to 80°W) were 1.23°C above average during August, beating the previous record of 1.01°C set in August 2005. August 2010 was the 7th straight record warm month in the tropical Atlantic. The five warmest months in history for the tropical Atlantic have all occurred this year; June 2005 comes in sixth place, and August 2010 in seventh. As I explained in detail in a post on record February SSTs in the Atlantic, the Arctic Oscillation (AO) and its close cousin, the North Atlantic Oscillation (NAO), are in large part to blame for the record SSTs, though global warming and Atlantic Multidecadal Oscillation (AMO) also play a role.

    The Bermuda-Azores High was weaker than average during August, which drove slower than usual trade winds over the tropical Atlantic. These lower trade wind speeds stirred up less cold waters from the depths than usual, and caused less evaporational cooling than usual, allowing August SSTs to remain at record warm levels. The Bermuda-Azores High and its associated trade winds are forecast to be at near-average strength during the next two weeks, according to the latest run of the GFS model. This means that Atlantic SST anomalies will continue to stay at record warm levels during September, significantly increasing the odds of major hurricanes in the Atlantic.


    Figure 2. The departure of sea surface temperature (SST) from average for September 9, 2010. Note the area of cool anomalies off the U.S. East Coast, due to the passage of Hurricane Earl. Cool anomalies are also evident east of Bermuda, due to the passage of Hurricane Danielle. Image credit: NOAA/NESDIS.
    "The ultimate judge of your swing is the flight of the ball." - Ben Hogan

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    12z Early Cycle NHC model tracks
    Invest92
    Statistical/Simple Models (CLIPER,BAMs,LBAR,other Statistical Models)





    Dynamic Models (More sophisticated models)







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