Meteorological history of Hurricane Florence: Difference between revisions
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==Landfall and dissipation== |
==Landfall and dissipation== |
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[[File:Hurricane Florence 2018 landfall animation.gif|thumb|right|NEXRAD animation of Hurricane Florence on September 13–14 as it made landfall in North Carolina.]] |
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⚫ | [[File:Hurricane Florence MPD 837.gif|thumb| |
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The outer rainbands of Hurricane Florence began affecting North Carolina during the latter half of September 13. Ample atmospheric moisture combined with strong upward lift from the anticyclone atop Florence yielded an environment conducive to widespread torrential precipitation. [[NEXRAD]] radar data from [[Morehead City, North Carolina|Morehead City]] (KMHX) indicated rainfall rates of {{convert|1|to|2|in|mm|abbr=on|round=5}} per hour within these bands.<ref>{{cite report|author=Joshua Weiss|publisher=Weather Prediction Center|date=September 13, 2018|accessdate=September 21, 2018|title=Mesoscale Precipitation Discussion: #0830|url=https://www.wpc.ncep.noaa.gov/metwatch/metwatch_mpd_multi.php?md=0830&yr=2018|type=Technical Discussion}}</ref> Florence's forward motion slowed throughout the day as the ridge steering it northwest built ahead of the cyclone toward the [[Appalachian Mountains]]. The previously disrupted eye rejuvenated; however, wind speeds within the storm continued to decrease.<ref>{{cite report|author=Stacy Stewart|publisher=National Hurricane Center|date=September 13, 2018|accessdate=September 21, 2018|title=Hurricane Florence Discussion Number 57|url=https://www.nhc.noaa.gov/archive/2018/al06/al062018.discus.057.shtml}}</ref> Additional fluctuations in the hurricane's core resulted in erratic movement, including a brief stalling period approximately 100 mi (155 km) east-southeast of [[Wilmington, North Carolina|Wilmington]].<ref name="D58">{{cite report|author=Stacy Stewart|publisher=National Hurricane Center|date=September 13, 2018|accessdate=September 21, 2018|title=Hurricane Florence Discussion Number 58|url=https://www.nhc.noaa.gov/archive/2018/al06/al062018.discus.058.shtml}}</ref><ref>{{cite report|author=Stacy Stewart|publisher=National Hurricane Center|date=September 13, 2018|accessdate=September 21, 2018|title=Hurricane Florence Advisory Number 58|url=https://www.nhc.noaa.gov/archive/2018/al06/al062018.public.058.shtml}}</ref> By 21:00 UTC, sustained hurricane-force winds reached the North Carolina coastline.<ref name="D58"/> Trudging west, the Florence ultimately made [[landfall]] near [[Wrightsville Beach, North Carolina|Wrightsville Beach]] at 11:15 UTC on September 14 as a Category 1 hurricane with winds of 90 mph (150 km/h) and a central pressure of 956 mbar (hPa; 28.23 inHg).<ref name="TCR"/> |
The outer rainbands of Hurricane Florence began affecting North Carolina during the latter half of September 13. Ample atmospheric moisture combined with strong upward lift from the anticyclone atop Florence yielded an environment conducive to widespread torrential precipitation. [[NEXRAD]] radar data from [[Morehead City, North Carolina|Morehead City]] (KMHX) indicated rainfall rates of {{convert|1|to|2|in|mm|abbr=on|round=5}} per hour within these bands.<ref>{{cite report|author=Joshua Weiss|publisher=Weather Prediction Center|date=September 13, 2018|accessdate=September 21, 2018|title=Mesoscale Precipitation Discussion: #0830|url=https://www.wpc.ncep.noaa.gov/metwatch/metwatch_mpd_multi.php?md=0830&yr=2018|type=Technical Discussion}}</ref> Florence's forward motion slowed throughout the day as the ridge steering it northwest built ahead of the cyclone toward the [[Appalachian Mountains]]. The previously disrupted eye rejuvenated; however, wind speeds within the storm continued to decrease.<ref>{{cite report|author=Stacy Stewart|publisher=National Hurricane Center|date=September 13, 2018|accessdate=September 21, 2018|title=Hurricane Florence Discussion Number 57|url=https://www.nhc.noaa.gov/archive/2018/al06/al062018.discus.057.shtml}}</ref> Additional fluctuations in the hurricane's core resulted in erratic movement, including a brief stalling period approximately 100 mi (155 km) east-southeast of [[Wilmington, North Carolina|Wilmington]].<ref name="D58">{{cite report|author=Stacy Stewart|publisher=National Hurricane Center|date=September 13, 2018|accessdate=September 21, 2018|title=Hurricane Florence Discussion Number 58|url=https://www.nhc.noaa.gov/archive/2018/al06/al062018.discus.058.shtml}}</ref><ref>{{cite report|author=Stacy Stewart|publisher=National Hurricane Center|date=September 13, 2018|accessdate=September 21, 2018|title=Hurricane Florence Advisory Number 58|url=https://www.nhc.noaa.gov/archive/2018/al06/al062018.public.058.shtml}}</ref> By 21:00 UTC, sustained hurricane-force winds reached the North Carolina coastline.<ref name="D58"/> Trudging west, the Florence ultimately made [[landfall]] near [[Wrightsville Beach, North Carolina|Wrightsville Beach]] at 11:15 UTC on September 14 as a Category 1 hurricane with winds of 90 mph (150 km/h) and a central pressure of 956 mbar (hPa; 28.23 inHg).<ref name="TCR"/> |
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As the hurricane moved ashore, deep convection blossomed along the eastern side of Florence's core. A strong inflow band became established within this area, resulting in localized heavy rain along the [[Crystal Coast]].<ref>{{cite report|author=Richard Otto|publisher=Weather Prediction Center|date=September 14, 2018|accessdate=September 21, 2018|title=Mesoscale Precipitation Discussion: #0834|url=https://www.wpc.ncep.noaa.gov/metwatch/metwatch_mpd_multi.php?md=0834&yr=2018|type=Technical Discussion}}</ref> Rainfall rates within the western eyewall reached an estimated {{convert|3|in|mm|abbr=on|round=5}} per hour while widespread accumulations of {{convert|1|to|2|in|mm|abbr=on|round=5}} per hour fell within the eastern band. A rain gage in [[Swansboro, North Carolina|Swansboro]] indicated accumulations of {{convert|14|to|15|in|mm|abbr=on}} by 14:34 UTC, exceeding radar estimations. Consistent flooding rains impacted [[Carteret County, North Carolina|Carteret County]], prompting a [[flash flood emergency]] by this time. Although the hurricane continued its slow movement west, the rain band gradually propagated east resulting in no net movement.<ref>{{cite report|author=David Roth|publisher=Weather Prediction Center|date=September 14, 2018|accessdate=September 21, 2018|title=Mesoscale Precipitation Discussion: #0836|url=https://www.wpc.ncep.noaa.gov/metwatch/metwatch_mpd_multi.php?md=0836&yr=2018|type=Technical Discussion}}</ref> Early on September 15, this band remained situated over [[Onslow County, North Carolina|Onslow]], Carteret, [[Jones County, North Carolina|Jones]], [[Lenoir County, North Carolina|Lenoir]], and [[Wayne County, North Carolina|Wayne]] counties. A new rain band developed closer to the storm's core over [[New Hanover County, North Carolina|New Hanover]], [[Brunswick County, North Carolina|Brunswick]], [[Pender County, North Carolina|Pender]], [[Bladen County, North Carolina|Bladen]], and [[Sampson County, North Carolina|Sampson]] counties. Catastrophic flash flooding from these bands ensued throughout the day, washing out roads and prompting water rescues.<ref>{{cite report|author=Richard Otto|publisher=Weather Prediction Center|date=September 15, 2018|accessdate=September 23, 2018|title=Mesoscale Precipitation Discussion: #0839|url=https://www.wpc.ncep.noaa.gov/metwatch/metwatch_mpd_multi.php?md=0839&yr=2018|type=Technical Discussion}}</ref> |
As the hurricane moved ashore, deep convection blossomed along the eastern side of Florence's core. A strong inflow band became established within this area, resulting in localized heavy rain along the [[Crystal Coast]].<ref>{{cite report|author=Richard Otto|publisher=Weather Prediction Center|date=September 14, 2018|accessdate=September 21, 2018|title=Mesoscale Precipitation Discussion: #0834|url=https://www.wpc.ncep.noaa.gov/metwatch/metwatch_mpd_multi.php?md=0834&yr=2018|type=Technical Discussion}}</ref> Rainfall rates within the western eyewall reached an estimated {{convert|3|in|mm|abbr=on|round=5}} per hour while widespread accumulations of {{convert|1|to|2|in|mm|abbr=on|round=5}} per hour fell within the eastern band. A rain gage in [[Swansboro, North Carolina|Swansboro]] indicated accumulations of {{convert|14|to|15|in|mm|abbr=on}} by 14:34 UTC, exceeding radar estimations. Consistent flooding rains impacted [[Carteret County, North Carolina|Carteret County]], prompting a [[flash flood emergency]] by this time. Although the hurricane continued its slow movement west, the rain band gradually propagated east resulting in no net movement.<ref>{{cite report|author=David Roth|publisher=Weather Prediction Center|date=September 14, 2018|accessdate=September 21, 2018|title=Mesoscale Precipitation Discussion: #0836|url=https://www.wpc.ncep.noaa.gov/metwatch/metwatch_mpd_multi.php?md=0836&yr=2018|type=Technical Discussion}}</ref> Early on September 15, this band remained situated over [[Onslow County, North Carolina|Onslow]], Carteret, [[Jones County, North Carolina|Jones]], [[Lenoir County, North Carolina|Lenoir]], and [[Wayne County, North Carolina|Wayne]] counties. A new rain band developed closer to the storm's core over [[New Hanover County, North Carolina|New Hanover]], [[Brunswick County, North Carolina|Brunswick]], [[Pender County, North Carolina|Pender]], [[Bladen County, North Carolina|Bladen]], and [[Sampson County, North Carolina|Sampson]] counties. Catastrophic flash flooding from these bands ensued throughout the day, washing out roads and prompting water rescues.<ref>{{cite report|author=Richard Otto|publisher=Weather Prediction Center|date=September 15, 2018|accessdate=September 23, 2018|title=Mesoscale Precipitation Discussion: #0839|url=https://www.wpc.ncep.noaa.gov/metwatch/metwatch_mpd_multi.php?md=0839&yr=2018|type=Technical Discussion}}</ref> |
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⚫ | [[File:Hurricane Florence MPD 837.gif|thumb|left|upright=1.5|[[Weather Prediction Center]] analysis of [[precipitable water]] at 20:20 UTC on September 14; values peaked at {{convert|2.6|in|mm|abbr=on}} near Morehead City, North Carolina. The magenta-shaded areas in eastern North Carolina indicate catastrophic flooding at the time of the graphic.<ref>{{cite report|author=David Roth|publisher=Weather Prediction Center|date=September 14, 2018|accessdate=September 23, 2018|title=Mesoscale Precipitation Discussion: #0837|url=https://www.wpc.ncep.noaa.gov/metwatch/metwatch_mpd_multi.php?md=0837&yr=2018|type=Technical Discussion}}</ref>]] |
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[[File:Hurricane Florence rainfall.png|thumb|left|A map of rainfall accumulations from September 13–18 across the Southeastern United States. The heaviest precipitation is concentrated in southeastern North Carolina where areas recorded more than {{convert|30|in|mm|abbr=on}}.]] |
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Although the center of Florence progressed inland over South Carolina, offshore [[convective available potential energy]] values of 1,000–2,000 J/kg and strong mid-level winds continued fueling the aforementioned rainbands.<ref>{{cite report|author=Richard Otto|publisher=Weather Prediction Center|date=September 15, 2018|accessdate=September 23, 2018|title=Mesoscale Precipitation Discussion: #0842|url=https://www.wpc.ncep.noaa.gov/metwatch/metwatch_mpd_multi.php?md=0842&yr=2018|type=Technical Discussion}}</ref> A low-risk of [[tornado]]es accompanied the heavy rain across North Carolina. Minimal diabatic heating stemming from the hurricane's lack of a thermal gradient kept the threat of tornadic storms low, with the primary driving force being ample atmospheric moisture.<ref>{{cite report|author=Andy Dean, Chris Broyles, and Nathan Wendt|publisher=Storm Prediction Center|date=September 14, 2018|accessdate=September 24, 2018|title=Sep 14, 2018 0600 UTC Day 1 Convective Outlook|url=https://www.spc.noaa.gov/products/outlook/archive/2018/day1otlk_20180914_1200.html}}</ref> Small-scale [[Training (meteorology)|training]] [[supercell]]s—series of severe storms that continuously develop, track across, and dissipate over the same areas—developed between Morehead City and Wilmington during the overnight hours of September 14–15.<ref>{{cite report|author=Andy Dean and Chris Broyles|publisher=Storm Prediction Center|date=September 14, 2018|accessdate=September 24, 2018|title=Sep 15, 2018 0100 UTC Day 1 Convective Outlook|url=https://www.spc.noaa.gov/products/outlook/archive/2018/day1otlk_20180915_0100.html}}</ref> |
Although the center of Florence progressed inland over South Carolina, offshore [[convective available potential energy]] values of 1,000–2,000 J/kg and strong mid-level winds continued fueling the aforementioned rainbands.<ref>{{cite report|author=Richard Otto|publisher=Weather Prediction Center|date=September 15, 2018|accessdate=September 23, 2018|title=Mesoscale Precipitation Discussion: #0842|url=https://www.wpc.ncep.noaa.gov/metwatch/metwatch_mpd_multi.php?md=0842&yr=2018|type=Technical Discussion}}</ref> A low-risk of [[tornado]]es accompanied the heavy rain across North Carolina. Minimal diabatic heating stemming from the hurricane's lack of a thermal gradient kept the threat of tornadic storms low, with the primary driving force being ample atmospheric moisture.<ref>{{cite report|author=Andy Dean, Chris Broyles, and Nathan Wendt|publisher=Storm Prediction Center|date=September 14, 2018|accessdate=September 24, 2018|title=Sep 14, 2018 0600 UTC Day 1 Convective Outlook|url=https://www.spc.noaa.gov/products/outlook/archive/2018/day1otlk_20180914_1200.html}}</ref> Small-scale [[Training (meteorology)|training]] [[supercell]]s—series of severe storms that continuously develop, track across, and dissipate over the same areas—developed between Morehead City and Wilmington during the overnight hours of September 14–15.<ref>{{cite report|author=Andy Dean and Chris Broyles|publisher=Storm Prediction Center|date=September 14, 2018|accessdate=September 24, 2018|title=Sep 15, 2018 0100 UTC Day 1 Convective Outlook|url=https://www.spc.noaa.gov/products/outlook/archive/2018/day1otlk_20180915_0100.html}}</ref> |
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Revision as of 18:58, 18 September 2019
Category 4 major hurricane (SSHWS/NWS) | |
![]() Track of Hurricane Florence | |
Formed | August 31, 2018 |
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Dissipated | September 18, 2018 |
(Extratropical after September 17) | |
Highest winds | 1-minute sustained: 150 mph (240 km/h) |
Lowest pressure | 937 mbar (hPa); 27.67 inHg |
Areas affected | |
Part of the 2018 Atlantic hurricane season |
The meteorological history of Hurricane Florence spanned 22 days from its inception as a tropical wave on August 28, 2018, to its dissipation on September 18.
Origins
On August 28, 2018, the National Hurricane Center (NHC) began monitoring a tropical wave—an elongated area of low air pressure—over Western Africa for possible tropical cyclogenesis over the subsequent five days as it progressed west.[1] Development into a tropical cyclone became increasingly likely the following day;[2] and a more defined low coalesced along the coast of Senegal on August 30.[3] On this day, the system split in two, with the northern one ultimately developing into Florence and the southern portion later becoming Tropical Depression Nineteen-E in the Eastern Pacific.[4] Favorable environmental conditions, including ample moisture and low wind shear,[5] enabled further organization and development of broad shower and thunderstorm activity. Lacking a well-defined center but posing an immediate threat to Cape Verde, the NHC began issuing advisories on the system as Potential Tropical Cyclone Six later that day.[nb 1] Easterly trade winds propelled the disturbance along a west to west-northwest trajectory.[7] Through much of the day and into August 31, convection remained confined to the southwest of the disturbance within a monsoon trough and precluded its classification as a tropical cyclone.[8] Toward the end of August 31, convective organization became sufficient for the NHC to mark the formation of Tropical Depression Six as the system passed south of Santiago in Cape Verde. Surface pressures on the island fell to 1005 mbar (hPa; 29.68 inHg) at 18:00 UTC.[9]
By September 1, the primary steering factor shifted to a strong, expansive subtropical ridge anchored well to the north. This ridge extended from Europe to the eastern United States and remained the dominant steering factor through much of the storm's history.[4] Moderate wind shear temporarily stunted development and displaced convection to the eastern side of the depression.[10] Pronounced banding features surrounded the circulation and the depression intensified to a tropical storm; accordingly the NHC assigned the system the name Florence.[11] Steady development marked the system's intensification. Satellite intensity estimates indicated Florence achieved maximum sustained winds of 60 mph (95 km/h) by 09:00 UTC on September 2.[12] Thereafter, shear and entrainment of dry air displaced convection from the surface low, leaving it exposed.[13] Considerable uncertainty in the forecast for Florence arose, as weather models began to depict various different solutions.[14] Fluctuations in organization and intensity continued through September 3.[15][16]
Unexpected intensification
Development of a small central dense overcast and a mid-level eye feature signified that Florence achieved hurricane strength early on September 4, roughly 1,240 miles (2,000 km) west-northwest of the Cape Verde islands.[17][18] Broad-scale conditions—moderate wind shear, sea surface temperatures below 81 °F (27 °C), and low relative humidity values—did not favor further intensification.[4] However, the system unexpectedly rapidly organized within a small area of low wind shear. Florence's small size enabled it to take advantage of this localized area.[19] The hurricane's core structure, eye, and outer banding improved markedly, catching forecasters off-guard and intensifying beyond model outputs.[20] In stark contrast to model guidance,[21] Florence continued to intensify and attained major hurricane status around 12:00 UTC on September 5. Sustained winds rose to 130 mph (215 km/h) and its pressure fell to 950 mbar (hPa; 28.05 inHg); this ranked it as a Category 4 hurricane on the Saffir-Simpson scale.[4] Situated at 22°42′N 46°36′W / 22.7°N 46.6°W,[22] Florence became the northernmost Category 4 hurricane east of 50°W.[23]
The hurricane's unforeseen intensification caused it to track farther north, out of the localized low shear.[24] Persistent shear finally took its toll on Florence on September 6 through September 7, causing convection to become asymmetrical and tilting the storm's core southwest to northeast.[25][26] By the early hours of September 7, rapid degradation of Florence's structure occurred. Its low-level circulation became exposed as convection became displaced to the northeast and the previously well-defined eye dissipated. Scatterometer data revealed the system weakened to tropical storm intensity by 00:00 UTC.[4][24] Meteorologist Robbie Berg described the intensity forecasts for Florence as a "self-defeating prophecy" owing to the "nuances of the environmental shear".[24][27] A building mid-level ridge halted Florence's northward movement, leading to a slow westward turn.[24][27] Weather models became increasingly consistent on the storm's future track, leading to greater confidence in a major impact to the Southeastern United States.[28] This threat was enhanced by the downstream effects of Typhoon Jebi's extratropical remnant influencing a ridge off the eastern United States which, in turn, forced a trough away from Florence faster than initially anticipated.[29] This trajectory proved climatologically unusual, with United States hurricane impacts primarily originating farther south and west of Florence's position on that day.[30]
United States approach
Environmental conditions became increasingly conducive to reorganization on September 8 as NOAA Hurricane Hunters began reconnaissance of the cyclone.[31] Convective banding blossomed around the storm and a formative eye appeared on satellite imagery.[32] The storm's central dense overcast became more defined and a complete eyewall developed within its core. Florence reattained hurricane-status around 12:00 UTC on September 9, with the Hurricane Hunters observing 76 mph (122 km/h) sustained winds at the surface.[4][33] Fueled by sea surface temperatures of 84.2 to 85.1 °F (29 to 29.5 °C), Florence rapidly intensified overnight. Convective bursts with frequent lightning surrounded the eyewall,[34] giving rise to a well-defined 12 mi (19 km) wide eye. Expanding outflow ventilated the cyclone, enabling continued growth.[35] The system rapidly achieved Category 4 intensity by 16:00 UTC, with reconnaissance aircraft recording surface winds near 130 mph (215 km/h) and a pressure of 946 mbar (hPa; 27.93 inHg).[36] The hurricane's motion accelerated and shifted northwest by this time, a trajectory it would maintain for several days.[35]
![](http://upload.wikimedia.org/wikipedia/commons/thumb/0/04/Dramatic_Views_of_Hurricane_Florence_from_the_International_Space_Station_From_9_12_%2842828603210%29.jpg/220px-Dramatic_Views_of_Hurricane_Florence_from_the_International_Space_Station_From_9_12_%2842828603210%29.jpg)
Hurricane Florence achieved its initial peak intensity late on September 10 with sustained winds of 140 mph (220 km/h) and a pressure of 940 mbar (hPa; 27.76 inHg).[4][nb 2] The extent of hurricane-force winds doubled in size and well-defined mesovortices rotated along the inner eyewall.[37] Slight weakening ensued thereafter as an eyewall replacement cycle started; convection surrounding the eyewall became ragged and the eye itself filled.[38][39] This processes completed the following day, with the newly formed eye spanning 35 mi (55 km) across. Extensive outflow became established over the cyclone, extending northwest and east, providing ample ventilation and deformation which enabled Florence to continue expanding.[40] The system intensified again and reached its peak intensity with winds of 150 mph (240 km/h) and a pressure of 937 mbar (hPa; 27.76 inHg) at 18:00 UTC.[4][nb 3] The future track of the hurricane became increasingly complex as it approached the Carolinas. A strengthening trough moving inland over the Pacific Northwest amplified ridging over the Northeastern United States and western Atlantic Ocean, steering Florence to the west-northwest. A collapse of steering currents was anticipated around the time of landfall on September 14, which would result in the hurricane meandering near the coast or just inland for a prolonged period of time.[41]
Fluctuations in the organization of Florence continued through the remainder of September 11 into September 12. Environmental conditions remained highly favorable for intensification and the NHC forecast the system to strengthen just below Category 5 status by September 13;[42] however, the system soon weakened and degraded to Category 3 status by 18:00 UTC.[43] Florence steadily grew in size during this time, with tropical storm-force winds extending 195 mi (315 km) by the end of September 12.[44] The hurricane's core soon unraveled on September 13 as mid-level wind shear increased and upwelling of colder water reduced available energy.[4] The hurricane's eyewall eroded entirely along the south side and convection became disrupted. Reconnaissance data revealed an ongoing eyewall replacement cycle, with a 25–35 mi (35–55 km) wide inner-core and 60–70 mi (95–110 km) wide outer-core. Furthermore, sustained surface winds fell to an estimated 110 mph (175 km/h), marking the cessation of Florence's tenure as a major hurricane.[45]
Landfall and dissipation
![](http://upload.wikimedia.org/wikipedia/commons/thumb/8/8a/Hurricane_Florence_2018_landfall_animation.gif/220px-Hurricane_Florence_2018_landfall_animation.gif)
The outer rainbands of Hurricane Florence began affecting North Carolina during the latter half of September 13. Ample atmospheric moisture combined with strong upward lift from the anticyclone atop Florence yielded an environment conducive to widespread torrential precipitation. NEXRAD radar data from Morehead City (KMHX) indicated rainfall rates of 1 to 2 in (25 to 50 mm) per hour within these bands.[46] Florence's forward motion slowed throughout the day as the ridge steering it northwest built ahead of the cyclone toward the Appalachian Mountains. The previously disrupted eye rejuvenated; however, wind speeds within the storm continued to decrease.[47] Additional fluctuations in the hurricane's core resulted in erratic movement, including a brief stalling period approximately 100 mi (155 km) east-southeast of Wilmington.[48][49] By 21:00 UTC, sustained hurricane-force winds reached the North Carolina coastline.[48] Trudging west, the Florence ultimately made landfall near Wrightsville Beach at 11:15 UTC on September 14 as a Category 1 hurricane with winds of 90 mph (150 km/h) and a central pressure of 956 mbar (hPa; 28.23 inHg).[4]
As the hurricane moved ashore, deep convection blossomed along the eastern side of Florence's core. A strong inflow band became established within this area, resulting in localized heavy rain along the Crystal Coast.[50] Rainfall rates within the western eyewall reached an estimated 3 in (75 mm) per hour while widespread accumulations of 1 to 2 in (25 to 50 mm) per hour fell within the eastern band. A rain gage in Swansboro indicated accumulations of 14 to 15 in (360 to 380 mm) by 14:34 UTC, exceeding radar estimations. Consistent flooding rains impacted Carteret County, prompting a flash flood emergency by this time. Although the hurricane continued its slow movement west, the rain band gradually propagated east resulting in no net movement.[51] Early on September 15, this band remained situated over Onslow, Carteret, Jones, Lenoir, and Wayne counties. A new rain band developed closer to the storm's core over New Hanover, Brunswick, Pender, Bladen, and Sampson counties. Catastrophic flash flooding from these bands ensued throughout the day, washing out roads and prompting water rescues.[52]
![](http://upload.wikimedia.org/wikipedia/commons/thumb/c/ca/Hurricane_Florence_MPD_837.gif/330px-Hurricane_Florence_MPD_837.gif)
Although the center of Florence progressed inland over South Carolina, offshore convective available potential energy values of 1,000–2,000 J/kg and strong mid-level winds continued fueling the aforementioned rainbands.[54] A low-risk of tornadoes accompanied the heavy rain across North Carolina. Minimal diabatic heating stemming from the hurricane's lack of a thermal gradient kept the threat of tornadic storms low, with the primary driving force being ample atmospheric moisture.[55] Small-scale training supercells—series of severe storms that continuously develop, track across, and dissipate over the same areas—developed between Morehead City and Wilmington during the overnight hours of September 14–15.[56]
Florence weakened below hurricane strength by 00:00 UTC on September 15. Its close proximity to the coastline enabled it to maintain its organization and only slowly degrade.[4] Throughout the majority of the day intense rainbands persisted over southern North Carolina, with six-hourly accumulations averaging 3 to 6 in (76 to 152 mm) in two bands extending from Brunswick to Bladen counties and Pender to Sampson counties.[57] Aided by an anticyclone, this band stretched across 350 mi (565 km) along the eastern side of Florence. The heaviest rains shifted to South Carolina early on September 16; estimated rainfall rates reached 2 to 3 in (51 to 76 mm) per hour in Dillon, Marion, and Marlboro counties.[58] The system finally weakened to a tropical depression over South Carolina by 18:00 UTC on this day, more than two days after it made landfall. Florence accelerated north along the western edge of the ridge previously steering it west. It eventually became extratropical over West Virginia on September 17.[4] Heavy rains propagated north along with the circulation center; however, rainbands extended from Virginia to South Carolina through September 17 with a narrow band of convection pivoting along the eastern slopes of the Appalachian Mountains. An approaching frontal system caused the remnant system to accelerate east, and ultimately resulted in its dissipation over Massachusetts on September 18.[4] Precipitation gradually subsided as the system weakened and the flooding threat lessened accordingly. Moderate rain with localized areas of heavy precipitation extended into Pennsylvania, New York, and southern New England on September 18.[59]
Notes
- ^ A Potential Tropical Cyclone is a storm system that is not yet a tropical cyclone but is anticipated to produce tropical storm or hurricane conditions on land within 48 hours.[6]
- ^ Dropsonde data at this time indicated peak winds of 184 mph (296 km/h) aloft; however, surface based observations by reconnaissance indicated surface winds to be significantly lower.[4]
- ^ Florence's peak intensity was based on a reduction of reconnaissance flight-level winds of 163–165 mph (262–266 km/h) at 12:23 UTC and continued improvement of the hurricane's inner core thereafter.[4]
References
- ^ Robbie Berg (August 28, 2018). Tropical Weather Outlook (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ Lixion Avila (August 29, 2018). Tropical Weather Outlook (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ Lixion Avila (August 30, 2018). Tropical Weather Outlook (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ a b c d e f g h i j k l m n o Stacy Stewart and Robbie Berg (May 30, 2019). Hurricane Florence (AL062018) (PDF) (Report). Tropical Cyclone Report. National Hurricane Center. Retrieved September 18, 2019.
- ^ Lixion Avila (August 30, 2018). Potential Tropical Cyclone Six Discussion Number 2 (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ "[National Hurricane Center Glossary: Potential Tropical Cyclone". National Hurricane Center. 2019. Retrieved September 18, 2019.
- ^ Lixion Avila (August 30, 2018). Potential Tropical Cyclone Six Discussion Number 1 (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ Robbie Berg (August 31, 2018). Potential Tropical Cyclone Six Discussion Number 4 (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ Lixion Avila (August 31, 2018). Tropical Depression Six Discussion Number 6 (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ Jack Beven (September 1, 2018). Tropical Depression Six Discussion Number 7 (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ Robbie Berg (September 1, 2018). Tropical Storm Florence Discussion Number 8 (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ David Zelinsky (September 2, 2018). Tropical Storm Florence Discussion Number 12 (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ Stacy Stewart (September 2, 2018). Tropical Storm Florence Discussion Number 13 (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ Michael Brennan (September 2, 2018). Tropical Storm Florence Discussion Number 14 (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ David Zelinsky (September 3, 2018). Tropical Storm Florence Discussion Number 16 (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ Michael Brennan (September 3, 2018). Tropical Storm Florence Discussion Number 17 (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ Robbie Berg (September 4, 2018). Hurricane Florence Discussion Number 21 (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ Robbie Berg (September 4, 2018). Hurricane Florence Advisory Number 21 (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ Robbie Berg and Jamie Rhome (September 5, 2018). Hurricane Florence Discussion Number 25 (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ Dave Roberts (September 5, 2018). Hurricane Florence Discussion Number 24 (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ Robbie Berg and Jamie Rhome (September 5, 2018). Hurricane Florence Discussion Number 26 (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ Robbie Berg and Jamie Rhome (September 5, 2018). Hurricane Florence Advisory Number 26 (Report). National Hurricane Center. Retrieved September 8, 2018.
- ^ Sam Lillo [@splillo] (September 5, 2018). "Intensity at 18z has been increased to 115kt -- #Florence is officially a category 4 hurricane. At 22.4N / 46.2W, this also makes #Florence the furthest north category 4 hurricane east of 50W ever recorded in the Atlantic" (Tweet). Retrieved September 9, 2018 – via Twitter.
- ^ a b c d Robbie Berg (September 6, 2018). Hurricane Florence Discussion Number 29 (Report). National Hurricane Center. Retrieved September 9, 2018.
- ^ Eric Blake (September 6, 2018). Hurricane Florence Discussion Number 27 (Report). National Hurricane Center. Retrieved September 9, 2018.
- ^ David Zelinsky (September 6, 2018). Hurricane Florence Discussion Number 28 (Report). National Hurricane Center. Retrieved September 9, 2018.
- ^ a b Eric Blake (September 7, 2018). Tropical Storm Florence Discussion Number 31 (Report). National Hurricane Center. Retrieved September 9, 2018.
- ^ Robbie Berg (September 7, 2018). Tropical Storm Florence Discussion Number 33 (Report). National Hurricane Center. Retrieved September 9, 2018.
- ^ Philippe Papin [@pppapin] (September 7, 2018). "A lot of huge track shifts we've seen the last 3-4 days are also related to the downstream impact of #Jebi's #ET. Big reconfiguration of the waveguide to favor a ridging on the east coast. That ridge kicked the first trough N of Florence out much faster than originally fcasted" (Tweet). Retrieved September 18, 2019 – via Twitter.
- ^ Michael Lowry [@MichaelRLowry] (September 7, 2018). "For historical perspective, most landfalling U.S. hurricanes have tracked much farther south and west of #Florence's current position" (Tweet). Retrieved September 9, 2018 – via Twitter.
- ^ Robbie Berg (September 8, 2018). Tropical Storm Florence Discussion Number 38 (Report). National Hurricane Center. Retrieved September 9, 2018.
- ^ Lixion Avila (September 9, 2018). Tropical Storm Florence Discussion Number 39 (Report). National Hurricane Center. Retrieved September 9, 2018.
- ^ Eric Blake (September 9, 2018). Hurricane Florence Discussion Number 41 (Report). National Hurricane Center. Retrieved September 9, 2018.
- ^ Stacy Stewart (September 10, 2018). Hurricane Florence Discussion Number 43 (Report). National Hurricane Center. Retrieved September 10, 2018.
- ^ a b Eric Blake (September 10, 2018). Hurricane Florence Discussion Number 44 (Report). National Hurricane Center. Retrieved September 10, 2018.
- ^ Eric Blake (September 10, 2018). Hurricane Florence Tropical Cyclone Update (Report). National Hurricane Center. Retrieved September 10, 2018.
- ^ Eric Blake (September 10, 2018). Hurricane Florence Discussion Number 46 (Report). National Hurricane Center. Retrieved September 12, 2018.
- ^ Jack Beven (September 11, 2018). Hurricane Florence Discussion Number 47 (Report). National Hurricane Center. Retrieved September 12, 2018.
- ^ Daniel Brown (September 11, 2018). Hurricane Florence Discussion Number 48 (Report). National Hurricane Center. Retrieved September 12, 2018.
- ^ Stacy Stewart (September 11, 2018). Hurricane Florence Discussion Number 49 (Report). National Hurricane Center. Retrieved September 12, 2018.
- ^ Stacy Stewart (September 11, 2018). Hurricane Florence Discussion Number 50 (Report). National Hurricane Center. Retrieved September 12, 2018.
- ^ Richard Pasch (September 12, 2018). Hurricane Florence Discussion Number 51 (Report). National Hurricane Center. Retrieved September 21, 2018.
- ^ Stacy Stewart (September 12, 2018). Hurricane Florence Intermediate Advisory Number 53A (Report). National Hurricane Center. Retrieved September 12, 2018.
- ^ Stacy Stewart (September 12, 2018). Hurricane Florence Advisory Number 54 (Report). National Hurricane Center. Retrieved September 21, 2018.
- ^ Jack Beven (September 13, 2018). Hurricane Florence Discussion Number 55 (Report). National Hurricane Center. Retrieved September 21, 2018.
- ^ Joshua Weiss (September 13, 2018). Mesoscale Precipitation Discussion: #0830 (Technical Discussion). Weather Prediction Center. Retrieved September 21, 2018.
- ^ Stacy Stewart (September 13, 2018). Hurricane Florence Discussion Number 57 (Report). National Hurricane Center. Retrieved September 21, 2018.
- ^ a b Stacy Stewart (September 13, 2018). Hurricane Florence Discussion Number 58 (Report). National Hurricane Center. Retrieved September 21, 2018.
- ^ Stacy Stewart (September 13, 2018). Hurricane Florence Advisory Number 58 (Report). National Hurricane Center. Retrieved September 21, 2018.
- ^ Richard Otto (September 14, 2018). Mesoscale Precipitation Discussion: #0834 (Technical Discussion). Weather Prediction Center. Retrieved September 21, 2018.
- ^ David Roth (September 14, 2018). Mesoscale Precipitation Discussion: #0836 (Technical Discussion). Weather Prediction Center. Retrieved September 21, 2018.
- ^ Richard Otto (September 15, 2018). Mesoscale Precipitation Discussion: #0839 (Technical Discussion). Weather Prediction Center. Retrieved September 23, 2018.
- ^ David Roth (September 14, 2018). Mesoscale Precipitation Discussion: #0837 (Technical Discussion). Weather Prediction Center. Retrieved September 23, 2018.
- ^ Richard Otto (September 15, 2018). Mesoscale Precipitation Discussion: #0842 (Technical Discussion). Weather Prediction Center. Retrieved September 23, 2018.
- ^ Andy Dean, Chris Broyles, and Nathan Wendt (September 14, 2018). Sep 14, 2018 0600 UTC Day 1 Convective Outlook (Report). Storm Prediction Center. Retrieved September 24, 2018.
{{cite report}}
: CS1 maint: multiple names: authors list (link) - ^ Andy Dean and Chris Broyles (September 14, 2018). Sep 15, 2018 0100 UTC Day 1 Convective Outlook (Report). Storm Prediction Center. Retrieved September 24, 2018.
- ^ Frank Pereira (September 15, 2018). Mesoscale Precipitation Discussion: #0845 (Technical Discussion). Weather Prediction Center. Retrieved September 23, 2018.
- ^ Richard Otto (September 16, 2018). Mesoscale Precipitation Discussion: #0848 (Technical Discussion). Weather Prediction Center. Retrieved September 23, 2018.
- ^ Richard Otto (September 18, 2018). Mesoscale Precipitation Discussion: #0860 (Technical Discussion). Weather Prediction Center. Retrieved September 18, 2019.