Hurricane Irene Adam Sobel, Suzana Camargo, Hui Shi, Columbia University
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Hurricane Irene Adam Sobel, Suzana Camargo, Hui Shi, Columbia University sual summary of Irene’s track, tensity, size and appearance Maximum wind, minimum pressure Satellite image when Irene was category 3 (near max intensity) Model forecasts Different curves show results from different computer models. These forecasts were made on August 24. The track was forecast remarkably well; the intensity forecasts tended to predict a stronger storm than actually occurred. Sea Surface Temperature A rule of thumb is that tropical cyclones need the SST to be at least 26C in order to form, or to maintain their strength. Satellite image just after NYC landfall Irene had become quite Asymmetric (non-circular) but still had an eye, despite being only tropical storm strength at this point Radar image at NYC landfall Rainfall was focused on the north side as Irene Encountered a cold front over land on its northwest flank. Wind field A full barb is 10 knots, half a barb is 5 knots; add up the barbs to get the wind speed at any point. 1 knot is 1.15 mph. This wind field is an estimate based on satellite imagery, from when Irene was over the New Jersey coast. Rainfall The left plot is from satellite estimates (in mm), the right is from rain gauges (which is why it shows nothing over the ocean). Both represent total accumulated rain from Irene’s passage. Storm surge This plot shows the water level measured by the tide gauge at the Battery. The peak storm surge was about 4 feet above the normal tide. It happened to be a Spring Tide, higher than usual anyway. Flooding The most devastating flooding, particular in upstate NY and New England, was from rainfall. This image shows the sediment plume in the Hudson River and NY harbor from all the flooded streams that drain into the Hudson. Have there been other storms like Irene? Yes. Floyd (1999) had a very similar track to Irene’s, shown above right. The 1938 Hurricane’s track is shown above left. That one was different because it came directly from the ocean, not making landfall before reaching the NY area as Irene and Floyd did. Because it moved fast, the 1938 storm was able to stay strong (category 3) as it came over the colder waters off Long Island. Irene moved much more slowly. Because of its large size and slow motion, it was clear early on that the danger in our area from Irene was rain and storm surge. Rainfall from Floyd Compare to Irene, on the middle panel.. 1938 Hurricane Floyd (1999)_
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Hurricane Irene Adam Sobel, Suzana Camargo, Hui Shi, Columbia University. Storm surge. Satellite image just after NYC landfall Irene had become quite Asymmetric (non-circular) but still had an eye, despite being only tropical storm strength at this point. This plot shows the water - PowerPoint PPT Presentation
Transcript of Hurricane Irene Adam Sobel, Suzana Camargo, Hui Shi, Columbia University
Hurricane Irene Adam Sobel, Suzana Camargo, Hui Shi, Columbia University
Visual summary of Irene’s track,intensity, size and appearance
Maximum wind,minimum pressure
Satellite image whenIrene was category 3 (near max intensity)
Model forecasts Different curves show results from different computer models. These forecasts were made on August 24.The track was forecast remarkably well; the intensity forecasts tendedto predict a stronger storm than actually occurred.
Sea Surface TemperatureA rule of thumb isthat tropical cyclonesneed the SST to beat least 26C in order to form, or to maintain their strength.
Satellite image justafter NYC landfallIrene had become quite Asymmetric (non-circular) but still had an eye, despite beingonly tropical storm strength atthis point
Radar image atNYC landfallRainfall was focused on thenorth side as Irene Encountered a cold front over land on its northwest flank.
Wind fieldA full barb is 10 knots, half a barb is5 knots; add up the barbs to get thewind speed at any point. 1 knot is1.15 mph. This wind field is anestimate based on satellite imagery,from when Irene was over the NewJersey coast.
RainfallThe left plot is from satellite estimates (in mm), the right is fromrain gauges (which is why it shows nothing over the ocean). Bothrepresent total accumulated rain from Irene’s passage.
Storm surgeThis plot shows the waterlevel measured by the tidegauge at the Battery. Thepeak storm surge was about4 feet above the normaltide. It happened to be aSpring Tide, higher than usual anyway.
FloodingThe most devastating flooding, particularlyin upstate NY and New England, was fromrainfall. This image shows the sediment plume in the Hudson River and NY harborfrom all the flooded streams that draininto the Hudson.
Have there been other storms like Irene?Yes. Floyd (1999) had a very similar trackto Irene’s, shown above right. The 1938Hurricane’s track is shown above left. That one was different because it came directlyfrom the ocean, not making landfall beforereaching the NY area as Irene and Floyddid. Because it moved fast, the 1938 stormwas able to stay strong (category 3) as itcame over the colder waters off Long Island.Irene moved much more slowly. Because ofits large size and slow motion, it was clear early on that the danger in our area fromIrene was rain and storm surge.
Rainfall from FloydCompare to Irene, on the middle panel..
1938 Hurricane Floyd (1999)_
