NyCwEaThErFeEn Posted September 10, 2018 Share Posted September 10, 2018 3 hours ago, Yaz said: What if Florence hits Florence (SC OR NC)? 1 hour ago, Stormlover74 said: What if Florence who lives on Florence Road in Florence NC gets hit by Florence? U guys are both dumb and that’s not funny people are going to die! Dumb ****s Link to comment Share on other sites More sharing options...
Stormlover74 Posted September 10, 2018 Share Posted September 10, 2018 9 minutes ago, NyCwEaThErFeEn said: U guys are both dumb and that’s not funny people are going to die! Dumb ****s Not if they evacuate as instructed Link to comment Share on other sites More sharing options...
NyCwEaThErFeEn Posted September 10, 2018 Share Posted September 10, 2018 Just now, Stormlover74 said: Not if they evacuate as instructed You know people are going to stay. Most people will leave but it happens every storm. I got a cousin in Wilmington and she and her family are driving 5 hours inland! Link to comment Share on other sites More sharing options...
BxEngine Posted September 10, 2018 Share Posted September 10, 2018 24 minutes ago, NyCwEaThErFeEn said: U guys are both dumb and that’s not funny people are going to die! Dumb ****s Time for another break tony... Link to comment Share on other sites More sharing options...
Rtd208 Posted September 11, 2018 Share Posted September 11, 2018 Not sure how reliable this poster is but I wanted to share it anyway. Link to comment Share on other sites More sharing options...
Rtd208 Posted September 11, 2018 Share Posted September 11, 2018 Link to comment Share on other sites More sharing options...
LongBeachSurfFreak Posted September 11, 2018 Share Posted September 11, 2018 You can see the much larger area of wind maximum after the EWRC. This acts to increase the swell generation potential. Winds above a certain speed aren’t very efficient in transferring energy into the ocean. So a small pin hole eye with say 160mph winds creates smaller seas then a large eye with winds of 130mph. So what that means for us is that a larger more powerful swell is on tap. With this large swell event comes more of a threat for beach washovers and erosion. Historically we have never had a storm this strong on this trajectory. I fully expect major coastal effects including some damage at our area beaches late this week. Link to comment Share on other sites More sharing options...
Cfa Posted September 11, 2018 Share Posted September 11, 2018 I was hoping we’d get some tropical rains from this, oh well. Any chance this hurricane inflicts WAR damage? Link to comment Share on other sites More sharing options...
Gravity Wave Posted September 11, 2018 Share Posted September 11, 2018 GFS caves completely. Is the Euro back to being the King? Link to comment Share on other sites More sharing options...
Dan76 Posted September 11, 2018 Share Posted September 11, 2018 Jeez.....NW winds 55 to 60 kt with gusts up to 140 kt. Seas 15 to 20 ft, subsiding to 13 to 18 ft after midnight. Showers. http://marine.weather.gov/MapClick.php?x=295&y=109&site=ilm&zmx=&zmy=&map_x=295&map_y=109#.W5f3yq3eCHs Link to comment Share on other sites More sharing options...
LibertyBell Posted September 11, 2018 Share Posted September 11, 2018 On 9/9/2018 at 5:23 PM, Cfa said: I remember reading an article/study which mentioned that the theoretical max for the NYC metro is a Cat 4. That or a high end Cat 3 would be our worst case scenario. Sandy wasn’t a joke, far from it, but it was a storm surge storm more than anything else. Sandy’s winds, while severe, were manageable. Rainfall wasn’t anything special with it either. You're right and so is LBSF about the track, it was calculated that our worst case scenario would be a hurricane tracking into Monmouth County, and the maximum possible wind speed that those waters can support was calculated to be 145 mph. A cat 4 may have reached our latitude and hit eastern New England when the Colonial Hurricane happened back in the 1600s, that one was said to be stronger than the 1938 hurricane. NYC may also have been hit by a Cat 4 back in pre Columbian times. That 1821 Hurricane really intrigues me and how was it able to maintain its strength with a track so close to the coast. Link to comment Share on other sites More sharing options...
LongBeachSurfFreak Posted September 11, 2018 Share Posted September 11, 2018 2 minutes ago, LibertyBell said: You're right and so is LBSF about the track, it was calculated that our worst case scenario would be a hurricane tracking into Monmouth County, and the maximum possible wind speed that those waters can support was calculated to be 145 mph. A cat 4 may have reached our latitude and hit eastern New England when the Colonial Hurricane happened back in the 1600s, that one was said to be stronger than the 1938 hurricane. NYC may also have been hit by a Cat 4 back in pre Columbian times. That 1821 Hurricane really intrigues me and how was it able to maintain its strength with a track so close to the coast. Great post! The great colonial hurricane is the gold standard for what’s possible at our latitude that we have direct evidence of. I say at our latitude because it most likely took a track over eastern LI and up into New England. That storm likely was a high end 3, so stronger the both 38 and carol which were low end 3’s. The pre Columbian sediment evidence is especially intriguing. Was it a hurricane? Nor’ Easter? Or possibly even a tsunami? We will never know, but the deposits point to something off the scale. Link to comment Share on other sites More sharing options...
LibertyBell Posted September 11, 2018 Share Posted September 11, 2018 4 hours ago, LongBeachSurfFreak said: You can see the much larger area of wind maximum after the EWRC. This acts to increase the swell generation potential. Winds above a certain speed aren’t very efficient in transferring energy into the ocean. So a small pin hole eye with say 160mph winds creates smaller seas then a large eye with winds of 130mph. So what that means for us is that a larger more powerful swell is on tap. With this large swell event comes more of a threat for beach washovers and erosion. Historically we have never had a storm this strong on this trajectory. I fully expect major coastal effects including some damage at our area beaches late this week. Is this why the surge with Katrina was much higher than its category? Also hurricanes that were Cat 5 once still maintain that surge for awhile even when they start to weaken Link to comment Share on other sites More sharing options...
LibertyBell Posted September 11, 2018 Share Posted September 11, 2018 10 minutes ago, LongBeachSurfFreak said: Great post! The great colonial hurricane is the gold standard for what’s possible at our latitude that we have direct evidence of. I say at our latitude because it most likely took a track over eastern LI and up into New England. That storm likely was a high end 3, so stronger the both 38 and carol which were low end 3’s. The pre Columbian sediment evidence is especially intriguing. Was it a hurricane? Nor’ Easter? Or possibly even a tsunami? We will never know, but the deposits point to something off the scale. Thanks and I was wondering about that too if it was a megatsunami that could even be from a meteorite hitting our coastal waters. We need a really fast moving storm to curve into the coast around the Atlantic Highlands in late August or September timed with the highest tides of the month (maybe around the equinox when the highest tides of the year are supposed to be- thats around when 1938 came in) in a really hot/humid summer with above normal rainfall prior to the storm to get the kind of high end storm worst case scenario we're talking about, not that we ever want to see something like that in our lifetimes. A trillion dollar disaster with probably even more lives lost than 911 A truly sobering thought on this day. Link to comment Share on other sites More sharing options...
LibertyBell Posted September 11, 2018 Share Posted September 11, 2018 On 9/9/2018 at 7:44 PM, qg_omega said: Getting a cat 4 coming in from the SE is almost impossible, pressure wise sandy was the strongest storm ever to hit our area. The size of the surge was also historic in terms of coastline impacted. Winds also remained on shore after landfall given it's landfall location and direction. All very unusual and historic Wow thanks for this- what track did you model for this- into Sandy Hook? And was the max wind speed modeled 145? It would be interesting to model the same track four different times, one with each category. edit- this was for Hailstorm sorry Link to comment Share on other sites More sharing options...
Rtd208 Posted September 11, 2018 Share Posted September 11, 2018 If anyone is interested Matt Lanza put together a list comprised of meteorologists, storm chasers etc. to be able to track Florence on Twitter. https://twitter.com/mattlanza/lists/florence Link to comment Share on other sites More sharing options...
bluewave Posted September 11, 2018 Share Posted September 11, 2018 2 hours ago, LibertyBell said: That 1821 Hurricane really intrigues me and how was it able to maintain its strength with a track so close to the coast. I just found a great presentation on the 1821 hurricane. https://ams.confex.com/ams/95Annual/webprogram/Paper257982.html Tuesday, 6 January 2015: 2:30 PM 128AB (Phoenix Convention Center - West and North Buildings) Megan E. Linkin, Swiss Re America Holding Corporation, Armonk, NY Recorded Presentation Hurricane Sandy, with its unique track, 1,000 mile wide wind field and low central pressure, pushed record breaking storm surge into the New York and New Jersey coasts, destroying businesses, homes and lives in a short 24 hour period. But for all the devastation and damage that Hurricane Sandy brought, its intensity at landfall, measured by 1-minute maximum sustained winds, was equivalent to a minimal Category 1 hurricane. Other events in recent years (Irene, Isabel, Gloria, Bob), while significant, weakened prior to landfall, coming onshore as either Category 1 or Category 2 hurricanes, and not the major hurricanes originally anticipated and feared. History, however, shows us that we may not always be as fortunate. The 1821 hurricane, commonly referred to as the Norfolk � Long Island hurricane, roared through the Mid-Atlantic and Northeastern United States in early September, passing over or near major cities and tourism regions such as the Outer Banks, Norfolk, Cape May and New York City. Coastal communities in North Carolina were washed away, ships in Norfolk, VA were pushed ashore and the Delaware Bay flooded Cape May, NJ. On eastern Long Island, the aftermath was described as, "the most awful and desolating ever experienced." The hurricane was a devastating event for the expanse of Northeast United States, with communities, farms and churches laid in ruins from North Carolina to New Hampshire. The hurricane is notable not only for its strength, but its contribution to science; it is the storm that led to the discovery that in the Northern Hemisphere, these weather systems rotate in a counterclockwise direction. With all existing documentation around the 1821 hurricane referring to a catastrophic, devastating event, and with today's models we can reconstruct a track for this hurricane to understand how it moved up coast, along with its wind field and storm surge field to determine what the loss potential is if the 1821 hurricane recurred today. Using Swiss Re's proprietary tropical cyclone model, a deterministic wind field and storm surge analogs are developed for the 1821 hurricane. The wind footprint calculated for the 1821 hurricane results in a large area of the Eastern Seaboard being affected by powerful winds and wind gusts; in parts of coastal North Carolina, the wind gusts are in excess of 150 mph, with wind gusts up to 130 mph reaching as far north as Connecticut. Storm surge values for the analog hurricanes range from 11 � 13 feet at The Battery, and up to 25 feet in Atlantic City, NJ. With trillions of dollars of residential, commercial and automotive exposure currently in the path of such a storm, the loss potential of the 1821 Norfolk-Long Island hurricane exceeds economic losses from other notable East Coast storms, including the 1938 Long Island Express and Hurricane Sandy. Physical economic losses are calculated to be in the range of USD 100 billion; actual economic losses, which include the intangibles, such as lost tax revenue and changes in asset values, are closer to USD 150 billion. It is imperative that we, as a nation and a society, look into the past to plan for the future, especially peering through the veil of climate change. Hurricanes Irene and Sandy served as harsh reminders that the Eastern Seaboard, particularly the Northeast US, is not immune to hurricane strikes. A recurrence of the 1821 Norfolk Long Island hurricane would be a paradigm shifter, severely and negatively impacting the economy and altering the culture of the oldest part of the United States going forward. Comprehending the potential consequences of historical storms today will help both improve our understanding of the "worst case event," and motivate those in coastal areas to take the necessary steps to prepare for all storms which are possible, even those beyond our current generations' memories. Link to comment Share on other sites More sharing options...
Rtd208 Posted September 11, 2018 Share Posted September 11, 2018 Still a decent chance we will see some rain early next week with the remnants of Florence. It is going to be amazing to watch this storm unfold over the Carolina's and even portions of Virginia the next 4-5 days. Hopefully everyone in that area stays safe. Link to comment Share on other sites More sharing options...
Brian5671 Posted September 11, 2018 Author Share Posted September 11, 2018 12 minutes ago, Rtd208 said: Still a decent chance we will see some rain early next week with the remnants of Florence. It is going to be amazing to watch this storm unfold over the Carolina's and even portions of Virginia the next 4-5 days. Hopefully everyone in that area stays safe. South Carolina now in the game with some models showing a SW drift right at or just prior to landfall. Link to comment Share on other sites More sharing options...
Rtd208 Posted September 12, 2018 Share Posted September 12, 2018 Found this a bit interesting. Link to comment Share on other sites More sharing options...
Rtd208 Posted September 12, 2018 Share Posted September 12, 2018 Link to comment Share on other sites More sharing options...
Stormlover74 Posted September 12, 2018 Share Posted September 12, 2018 Link to comment Share on other sites More sharing options...
Rtd208 Posted September 12, 2018 Share Posted September 12, 2018 Link to comment Share on other sites More sharing options...
LibertyBell Posted September 12, 2018 Share Posted September 12, 2018 5 hours ago, bluewave said: I just found a great presentation on the 1821 hurricane. https://ams.confex.com/ams/95Annual/webprogram/Paper257982.html Tuesday, 6 January 2015: 2:30 PM 128AB (Phoenix Convention Center - West and North Buildings) Megan E. Linkin, Swiss Re America Holding Corporation, Armonk, NY Recorded Presentation Hurricane Sandy, with its unique track, 1,000 mile wide wind field and low central pressure, pushed record breaking storm surge into the New York and New Jersey coasts, destroying businesses, homes and lives in a short 24 hour period. But for all the devastation and damage that Hurricane Sandy brought, its intensity at landfall, measured by 1-minute maximum sustained winds, was equivalent to a minimal Category 1 hurricane. Other events in recent years (Irene, Isabel, Gloria, Bob), while significant, weakened prior to landfall, coming onshore as either Category 1 or Category 2 hurricanes, and not the major hurricanes originally anticipated and feared. History, however, shows us that we may not always be as fortunate. The 1821 hurricane, commonly referred to as the Norfolk � Long Island hurricane, roared through the Mid-Atlantic and Northeastern United States in early September, passing over or near major cities and tourism regions such as the Outer Banks, Norfolk, Cape May and New York City. Coastal communities in North Carolina were washed away, ships in Norfolk, VA were pushed ashore and the Delaware Bay flooded Cape May, NJ. On eastern Long Island, the aftermath was described as, "the most awful and desolating ever experienced." The hurricane was a devastating event for the expanse of Northeast United States, with communities, farms and churches laid in ruins from North Carolina to New Hampshire. The hurricane is notable not only for its strength, but its contribution to science; it is the storm that led to the discovery that in the Northern Hemisphere, these weather systems rotate in a counterclockwise direction. With all existing documentation around the 1821 hurricane referring to a catastrophic, devastating event, and with today's models we can reconstruct a track for this hurricane to understand how it moved up coast, along with its wind field and storm surge field to determine what the loss potential is if the 1821 hurricane recurred today. Using Swiss Re's proprietary tropical cyclone model, a deterministic wind field and storm surge analogs are developed for the 1821 hurricane. The wind footprint calculated for the 1821 hurricane results in a large area of the Eastern Seaboard being affected by powerful winds and wind gusts; in parts of coastal North Carolina, the wind gusts are in excess of 150 mph, with wind gusts up to 130 mph reaching as far north as Connecticut. Storm surge values for the analog hurricanes range from 11 � 13 feet at The Battery, and up to 25 feet in Atlantic City, NJ. With trillions of dollars of residential, commercial and automotive exposure currently in the path of such a storm, the loss potential of the 1821 Norfolk-Long Island hurricane exceeds economic losses from other notable East Coast storms, including the 1938 Long Island Express and Hurricane Sandy. Physical economic losses are calculated to be in the range of USD 100 billion; actual economic losses, which include the intangibles, such as lost tax revenue and changes in asset values, are closer to USD 150 billion. It is imperative that we, as a nation and a society, look into the past to plan for the future, especially peering through the veil of climate change. Hurricanes Irene and Sandy served as harsh reminders that the Eastern Seaboard, particularly the Northeast US, is not immune to hurricane strikes. A recurrence of the 1821 Norfolk Long Island hurricane would be a paradigm shifter, severely and negatively impacting the economy and altering the culture of the oldest part of the United States going forward. Comprehending the potential consequences of historical storms today will help both improve our understanding of the "worst case event," and motivate those in coastal areas to take the necessary steps to prepare for all storms which are possible, even those beyond our current generations' memories. Wow 25 feet at Atlantic City rivals Katrina. Hailstorm's modeling showed a worst case scenario delivering a 33 foot storm surge to Southern Queens which would exceed Katrina by a few feet. With all these stalling hurricanes we've had recently due to anomalous blocking I wonder if we might need to revise our idea of a worst case scenario- what if a powerful Cat 3/4 came close to landfall in Central NJ and just stalled there, a la Dec 1992 noreaster or Ash Wednesday 1962 storm or Harvey or what Florence might do? It would slowly weaken but the surge and wind over many high tide cycles would be truly catastrophic and the feet of rainfall! Link to comment Share on other sites More sharing options...
LibertyBell Posted September 12, 2018 Share Posted September 12, 2018 On 9/9/2018 at 6:08 PM, Hailstorm said: I definitely agree with this. According to the SLOSH models I have just run, parts of Brooklyn and Queens could get slammed with up to a 32-foot storm tide in a Cat. 4, assuming the impact coincides with high tide. Sandy, by comparison, "only" produced a storm tide of 11 feet in Manhattan. This would make Sandy appear to be "child's play" if that scenario came into fruition; as the surge would penetrate at least 3 miles further inland along the south-facing shorelines of Brooklyn, Queens and Long Island. Wow almost 34 ft near Southern Queens, I wonder why it's less in Southern Nassau? Was this from a track modeled into Sandy Hook of a 145 mph hurricane? It would be interesting to see the same track modeled with different intensity hurricanes from 1-4. Also with the new climate regime of stalling hurricanes I wonder how much worse it would be to have a Cat 3/4 stall right along the coast, similar to what the Dec 1992 noreaster or the Ash Wednesday 1962 storm or what Harvey did or what Florence might do. Link to comment Share on other sites More sharing options...
Rtd208 Posted September 12, 2018 Share Posted September 12, 2018 Link to comment Share on other sites More sharing options...
Rtd208 Posted September 12, 2018 Share Posted September 12, 2018 Link to comment Share on other sites More sharing options...
NJwx85 Posted September 12, 2018 Share Posted September 12, 2018 Still too early to determine if we will receive any impacts up here at all except for beach erosion, however the remnants should eventually merge with a trough which will swing through here early next week. Unless of course Florence ends up taking a wild track and ends up further Southwest than forecasted. Link to comment Share on other sites More sharing options...
gravitylover Posted September 12, 2018 Share Posted September 12, 2018 In the latest visible shot this really is a beautiful storm. Knowing (approximately) what's going to happen over the next few days I hate appreciating it but I can't help it. Someone on the north side of the Chesapeake area-MD/DEL/NJ coast is getting a heckuva surf day today. Link to comment Share on other sites More sharing options...
tdp146 Posted September 12, 2018 Share Posted September 12, 2018 On 9/9/2018 at 6:08 PM, Hailstorm said: I definitely agree with this. According to the SLOSH models I have just run, parts of Brooklyn and Queens could get slammed with up to a 32-foot storm tide in a Cat. 4, assuming the impact coincides with high tide. Sandy, by comparison, "only" produced a storm tide of 11 feet in Manhattan. This would make Sandy appear to be "child's play" if that scenario came into fruition; as the surge would penetrate at least 3 miles further inland along the south-facing shorelines of Brooklyn, Queens and Long Island. Did you send the NWS your email address via this page in order to get access to run that model? https://slosh.nws.noaa.gov/sloshPub/disclaim.php Link to comment Share on other sites More sharing options...
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