List of paleotempestology records explained

See main article: Paleotempestology.

Paleotempestology is the study of past tropical cyclone activity by means of geological proxies as well as historical documentary records. The term was coined by American meteorologist Kerry Emanuel.

Examples

Place Country/state Data sources Duration of the record, in years Conclusions Sources Approximate coordinates
AD 1977 – 2000 Strong correlation of hits by named tropical cyclones with isotope ratio variations17.1175°N -88.8905°W
Sediments from floods 1,800 Low storm activity in the last 500 years, probably correlated to the Little Ice Age but continuing into the 19th and 20th century43.0914°N 131.449°W
Angliers PondFloridaLake sedimentsAD 1920Three storm deposits, linked presumably to Hurricane Donna, Great Miami Hurricane and 1921 Tampa hurricane26.42°N -82.06°W
JapanRiver terraces formed by typhoon flooding 11,600 Intense flooding during the late glacial to 5,000 – 4,500 years ago indicate increased typhoon activity, followed by a period of less intense activity until about 2,350 years ago35°N 140°W
Bay Jimmy Louisiana Seafloor sediments 1,200 years Four intense storms, including two recent ones[1] 29.4518°N -89.9007°W
Sediments in a coastal lagoon 5,000 Inactive period between 2,500 – 1,500 years, preceded and followed by more active periods 17.6362°N -61.8793°W
Basin Bayou Florida Overwash and inundation deposits 2,000 Over twice as active as today 900–1050 CE, with less activity 250 - 650 CE and 1150 - 1850 CE 30.4897°N -86.2463°W
Belize, central Overwash deposits 5001.2-1 catastrophic storms per century including one very strong storm before 1500AD17°N -103°W
Belize, south-central Sediments 7,000 Several active periods, between 6,900 – 6,700, 6,050 – 5,750, 5,450 – 4,750, 4,200 – 3,200, 2,600 – 1,450 and 600 – 200 years ago16.9°N -88.3°W
Tree ring evidence of storm damageAD 1700–present 25°N -80°W
Sand deposits in sinkhole 3,000 A stage without intense storms between 2,900 – 2,500 years ago, followed by an active period that lasted until 1,000 years ago. Two intense events about 500 years ago and an increase between 300 – 100 years ago 27°N -78°W
Brigantine, New JerseyNew JerseySediments1,500Two strong storms between 600–700 and 700–1,400 AD; nor'easters are also recorded here39.4019°N -74.3644°W
Cenote Chaltun Ha Mud layers in speleothems AD 365 – 2007 20.46°N -89.17°W
Commerce Bight Lagoon Sediment cores 7,000Active periods between 600 and 200, 1,450 – 2,600, 3,200 – 4,200, 4,750 – 5,450, 5,750 – 6,050 years ago16.8333°N -108°W
Sediments8,000Increased activity between 3,000 – 2,000 years ago and also during El Nino-leaning periods26.8333°N -87°W
Washover deposits Cyclone Mala and two older tropical cyclones[2] 16.9475°N 94.3703°W
Chenier PlainLouisianaSediments in coastal plain6007 hurricanes with category 3 or more intensity are known in the last 600 years, giving a frequency of 1.2 storms per century. Among the storms are Hurricane Audrey and Hurricane Rita29.7649°N -93.8004°W
Chezzetcook Inlet Sediment analysis1,000Potential storm deposits at 1200 AD, AD 1831 and AD 1848, the middle of which is correlated to a major storm; also an inactive phase in the 1950s and 1970s 44.7036°N -63.2583°W
QueenslandBeach ridges5,740Low activity between 1,820 – 850 and 2,580 – 3,230 years ago-17.6551°N 146.0598°W
Tree rings AD 1771 – 2014 Low activity in 1815–187534.972°N -77.119°W34.743°N -76.985°W
Sediment deposits 2,200 Several sand layers may correlate to hurricanes, including one perhaps linked to the 1867 San Narciso hurricane18.3206°N -65.2364°W
QueenslandBeach ridges 6,000 22 hits by intense storms in 6,000 years, implying return periods of 280 years-18.6701°N 146.5355°W
Reconstruction of annual tropical cyclone rainfall totals, which exhibits a decrease after a major volcanic eruption. Presently the oldest paleohurricane reconstruction using tree rings. 31.08°N -89.08°W
DurbanSouth AfricaSubmarine depositsHoloceneIncreased storminess during the early Holocene and during times with strong Indian Ocean Dipole activity-29.9°N 31°W
Duri Island Shell-gravel deposits1,30034.3333°N 126.6056°W
EshanessBoulders perched on cliffs 1,400Probably not tropical cyclones, but intense storm activity occurred since AD 1950, between 1,300 and 1,900 AD, 700–1,050 AD and 400 – 550 AD60.5°N -1.5°W
Australia, northwestern Washover fans 3,000 Tropical cyclone strikes took place 170 – 180 ± 16, 360 ± 30, 850 – 870 ± 60, 1,290 – 1,300 ± 90, 1,950 – 1,960 ± 90, 2,260 – 2,300 ± 120 and 2,830 – 2,850 ± 120 years ago, consistent with expectations based on sea surface temperature variations[3] -22.25°N 114.2325°W
NicaraguaSediment deposits5,400Last 800 years have an active climate with a return period of about 140–180 years, while between 800 and 2,800 the return period was only once between 600 and 2,100 years and another quiet period between 4,900 – 5,400 years ago; between 2,800 and 4,900 no records12.112°N -124.42°W
Back-barrier marshes 4,600 The last 4,600 years may have seen 27 storms, as well as 11 major storms in the last 3,300 years32.6677°N -80.0005°W
Coastal ridges and coral mortality 510 Active periods are known from 1980 to 2000, 1940–1960, 1860–1880, 1800–1830, 1760–1780, 1700–1720, 1630–1650, 1570–1590-17.2181°N 146.0681°W
France France Tempestites Inapplicable
Gales PointBelizeSediment cores5,500In the last 5,500 years 16 major hurricanes17.1667°N -103°W
Grand CaseSt. MartinSediments4,280Active period between 3,700 – 1,800 years ago, while 1,800 –800 years ago was inactive18.0833°N -68°W
Sediments 900-2,011 ADSubdued activity between 900-1350 and after 1950AD during the recent warm periods and Medieval Climate Anomaly, with increased activity during the Little Ice Age7.8936°N -76.6183°W
Coarse sediment deposits 7,000Active periods occurred within the last 50 years, between 1,200 and 500 years ago, 2,400 – 1,800 years ago and 4,600 – 3,800 years ago, with low activity before 4,400 years25°N -80°W
Overwash deposits1,885Active periods between 800 and 500, 1,300 – 900 or 650 – 1,200 years ago and coinciding with the Medieval Warm Period17.316°N -87.5351°W
AustraliaBeach ridges7,500Low activity/intensity between 5,500 and 3,500, 2,700–1,800 and 1,000–500 years ago, the former coinciding with the Neoglacial-14.1257°N 134.2764°W
Beach ridges and a coastal marsh 8,000 18 typhoon strikes in the last 8,000 years, with increased activity in the mid-Holocene until 3,900 years ago (2–5 times more storms) either due to a warmer climate or higher sea level induced better sensitivity to storms12°N 100°W
Deposits in lakes 350 1–2 typhoons per decade, with higher solar activity, positive Pacific Decadal Oscillation, La Nina and positive North Atlantic Oscillation correlating with decreases18.4167°N 112°W
Coastal dunes 3,4008 storms in 1095 ± 90 BC, 900–1000 BC, 975 ± 50 AD, 1720 ± 20 AD, 1740 ± 35 AD, 1790 ± 25 AD, 1850 ± 15 AD, and 1895 ± 10 AD19.1498°N 108.8116°W
Tempestite Increased tropical cyclone activity during the hot Toarcian Oceanic Anoxic EventInapplicable
Cay Sal BankBahamasSubaqueous sediments530On average 18.7-20.6 category 1+ storms per century. 34 storms between 770 to 1870 CE, only 8 between 1916 and 201623.875°N -79.75°W
Ilan Plain River erosion sediments in a lake2,000 Between 500 – 700 and after AD 1400 intense typhoon rainfall24.6°N 157°W
Oxygen isotope ratios in rocks Intense tropical cyclone activity in the Tethys until its closure 20 million years agoInapplicable
Tidal flat deposits 2,000 ENSO and ITCZ influences; anticorrelation between Japan/Korea and SE China typhoon activity 33.5°N 121°W
Kamikoshiki-jimaJapanSediments in coastal lagoons6,400Higher typhoon activity at the time of the Kamikaze typhoons, with high activity between 3,600 – 2,500 and between 1,000 – 300 years ago31.8333°N 179°W
Overwash deposits 1,000 26.0456°N -81.8116°W
Flood deposits in stalagmites 2,200Moderate activity between 1,450 – 850 AD and low activity between 500 – 850 and 1,450 – 1,650 AD-15.18°N 128.37°W
Beach ridges 3,200 Strong storms (at least Category 4 or Category 5) occur every 253 years -24.1131°N 152.7106°W
Laguna Alejandro Dominican RepublicSediment analysis910Strikes 910, 800, 730, 530, 500, 330, 260, 210, 200 and 170 years ago18.3131°N -71.0308°W
Laguna NegraNicaraguaDeposits in a coastal lake8,000One very strong storm ("Hurricane Elisenda") 3,340 ± 50 years ago, at the same time as increased storm activity in Alabama and Florida 12.045°N -83.9276°W
Storm deposits 3350 BC–AD 1050 0.46% probability of landfall any given year26.6848°N -97.5397°W
Overwash sediments5,0000.48% probability of landfall any given year, but an active period in the last 250 years and previous active periods between 2,500 – 1,000 and 3,600 – 5,400 years ago. El Nino is linked with lower activity, a strong West African Monsoon with higher activity18.09°N -65.52°W
Lake DaijaJapanSediments in a coastal lagoon2,000Beginning at 250 AD increased activity, while a quiet period has lasted from 1600 AD to today. Typhoon Jean, Typhoon Grace and others have been identified, including two deposits that may correlate to the Kamikaze typhoons which also coincide within an active period. Recorded storms appear to be of category 3 or higher strength32.24°N 129.98°W
Storm deposits4,80011 intense storms between 3,500 and 700 years ago, a quiet period before 3,200 radiocarbon years ago may be either a stage of inactivity or a change in the lake environment. Comparisons to Hurricane Frederic and Hurricane Ivan imply that the intense storms reached category 4 or 5 intensity30.25°N -127°W
Minerals from simultaneous seawater intrusion and island erosion3,500Two storms between 3,200 – 2,800 and 200 years ago -21.95°N -214°W
Hong Kong Marine sediments1,200Increased storm intensity during the Medieval Warm Period, with more but possibly weaker storms during the Little Ice Age and an increase in storm intensity after it22.12°N 113.53°W
Storm deposits3,500Between 3,100 – 1,800 years ago only weak activity, followed and preceded by strong activity; intense storms about once every ten years in the last 3,500 years and the storm activity correlates to sea surface temperatures16.4667°N 146°W
AlabamaOverwash deposits1,200[4] 30.273°N -123.92°W
Little Sippewissett MarshMassachusettsOverwash deposits400Annual landfall probability is about 2.3%, 4% in the last 50 years41.5°N -101°W
New YorkOverwash deposits3,500Increased activity during the Little Ice Age and an inactive period between 900 and 250 years ago40.59°N -73.6°W
Long Island blue holeBahamasDeposits in blue holes1,050Active between 1,245–1,290, 1,395–1,500, 1,590–1,650 and 1,775–1,845 AD in particular the most recent period. Inactive during 1,161–1,213, 1,528–1,585, 1,651–1,713, 1,877–1,927 and 1,933–2,003 AD23.265°N -75.117°W
Varves formed by post-storm sedimentation1000Up to eight Category 2–3 hurricanes occurred per century in the 12th to 16th century, while the preceding and the two subsequent ones only saw 2–3 such storms per century42.4267°N -79.8°W
Manatee BayJamaicaMultideposits1,200Four overwash deposits, one of which probably from a tsunami and the most recent one from Hurricane Ivan and Hurricane Dean17.8432°N -76.9861°W
Bermuda Lagoon deposits 1,600 years Increased activity between 1,200 - 1,800 AD[5]
Mattapoisett MarshMassachusettsStorm inundation deposits2,200Inactive period between 2,200 and 1,000 followed by an active period in the last 800 years41.5°N -71°W
China Storm deposits80,000Marine isotope stage 5e storm frequency comparable to that of Holocene low-latitude China37.9422°N 120.6766°W
Turks and Caicos IslandsSedimentsPast 1,520 yearsMaximum activity between 1,550-1,900 with 8 events/century. Active periods in 690-760, 960-1,100, 1,550-1,900 and inactive ones in 98-595, 618-690, 758-813, 831-901, 1,444-1,514 and 1,961-2,017 AD21.72°N -71.81°W
Sediments in a sinkhole4,500Active periods with intense storms 650 – 750 years ago, 925 – 875 years ago, 1,250 – 1,150 years ago, 2,800 – 2,300 years ago, 3,350 – 3,250 years ago, 3,600 – 3,500 years ago and 3,950 – 3,650 years ago; the maximum occurrence rate between 2,300 and 2,800 years ago saw six storms per century while the last 150 years have been fairly inactive. Mullet Pond records also somewhat weaker storms and shows a recurrence rate of 3.9 events per century.30°N -84.5°W
Backbarrier deposits 1,500 Poor preservation; only 5–8 deposits in 1,500 years 34°N -77°W
Sand layers in organic deposits 1,250One of the earliest paleotempestological records; nine sand layers were interpreted as evidence for hurricanes 41.679°N -69.9771°W
Sediments 4,500 (radiocarbon years)Storms occur about all 300 years; hyperactive period between 3,800 and 1,000 years ago30.3625°N -88.6235°W
Sediments 4,500 (radiocarbon years)Storms occur about all 300 years; hyperactive period between 3,800 and 1,000 years ago
Pinqing LagoonGuangdong Province, ChinaSediments1,850 CE - presentSeven typhoons in 130 years22.77°N 115.4°W
Playa Los Cocos Baja California Sur, MexicoSedimentsOne tsunami 530 BP and hurricanes 770, 600, 280 and 0 (Hurricane Olivia most likely) BP26.45°N -111.55°W
Beach ridges 3,000 12 hits by intense storms in 6,000 years, implying return periods of 180 years-14.4167°N 143.9825°W
Stalagmites 8002 strong storms between AD 1400 – 1600 after two centuries without one, seven strong storms between AD 1600 and AD 1800 and only one strong storm after that-17.2°N 144.6°W
Sediments in lake800Storms at 1475, 1530, 1575, 1670 and Hurricane Juan. The record probably reflects storms of at least category 244.6519°N -79.631°W
Sand ridges 5,000 Intense storms occurred between 130 and 1,550 years ago as well as between 3,380 – 5,010 years ago, while the time between 1,550 – 2,280 years ago had very weak storms -18.0333°N 149°W
Sediments in a lake 2,00035 hurricanes with active periods between 150 -1,150 AD and 1,400 – 1,675 AD; one historical hurricane (Hurricane Bob) recorded; some storms are stronger than the most intense hurricane there, the Great Colonial Hurricane of 1635
Lake sediments4,000Increased storm activity between 3,400 and 1,000 years ago. Recurrence rate of strong hurricanes appears to be much less than the historical rate, which may be due to measurement issues24.0833°N -104°W
Deposits in a coastal lagoon 4,000Active periods occurred between 2,600 – 1,800 years ago and between 500 and 250 years ago19.9486°N -76.5395°W
Coral bouldersNorthward migration of typhoon activity during the recent warm period15.155°N 117.65°W
Scrub IslandLagoon deposits 1,600 Two tsunami deposits, one of which linked to the 1755 Lisbon earthquake. Of the 23 remaining deposits most likely linked to hurricanes, one probably belongs to Hurricane Dog in 1950 and another to an unnamed hurricane in 1923. Increased activity in 445–525, 720–835, 1080–1230, 1625–1695, 1745–1890 and 1920–1970 including the Medieval Warm Period and decreased activity in 560, ~670, 965–1020,1400–1600, ~1740 cal. CE. 18.3333°N -63°W
New JerseySedimentsAD 214 – presentStorm deposits were emplaced between AD1875-1925, before AD1827, before AD1665-1696, in the 14th–15th century, before AD950-1040, AD429-966 and before AD260-52039.3167°N -94°W
South KoreaTree ringsAS 1,652 - 2,005Decreasing landfalling storms after volcanic eruptions. High activity between 1993 and 199738.1667°N 148°W
New YorkOverwash deposits300Severe storm surges associated with the 1821 Norfolk and Long Island hurricane and Hurricane Sandy40.5645°N -74.2869°W
Shell beach ridge 6,000An inactive period between about 5,400 and 3,700 years ago accompanied by drought. Storm intensity indicated by the ridges is about category 2–4 on the Saffir-Simpson scale, while no case of category 5 is inferred-26.5°N 113.6°W
Shark River SloughFloridaSediment cores4,600Decrease of storm activity after 2,800 years ago25.6559°N -80.7103°W
Shark River SloughFloridaSediment cores3,500Active periods 3,400–3,000, 2,200–1,500, 1,000–800, 600–300, and ~150–0 years ago25.3528°N -81.1144°W
Sediments Older than 1938ADSeveral historical deposits by the 1938 New England hurricane, Hurricane Carol, either Hurricane Donna or Hurricane Esther and the Ash Wednesday Storm of 196240.83°N -72.53°W
Shotgun Pond Florida Overwash and inundation deposits 2,000 Higher activity than the historical period 650–1000, 1100–1300, 1350–1450, and 1750–1850 AD, and lower activity than today 450–650, 1000–1100, 1300–1350, and 1500–1750 AD; Hurricane Michael in 2018 left a deposit29.9316°N -84.355°W
Sediments in tidal deposits 3,500Historical storms like Hurricane Hazel and Hurricane Hugo are recorded, with more storms until 1050 BC. Between 3050 and 1050 BC there are no storm deposits, but one deposit dating to 3750 BC appears to relate to a very intense event, perhaps due to a warmer climate at that time33.7554°N -78.812°W
Overwash deposits and microfossils 2,500 30.2516°N -89.4279°W
Deposits in blue holes 1,500 Mainly intense tropical cyclones recorded, including unnamed 1919 and 1945 Category 3 hurricanes although a weaker storm in 1945 might have also contributed. In general there are phases of high and low activity associated with phase changes of the ITCZ volcanic activity and the Little Ice Age23.78°N -77.69°W
Sediment cores +3,000 7 storms in 3,300 years, equating a recurrence rate of 1 every 471 years. An active period ended 1,100 years before present31.628°N -81.2285°W
Storm layers4,500 An active period between about 600 and 1,700 years ago, but fewer major hurricanes in the last 600 years30°N -84.5°W
Succotash MarshRhode IslandSediment overwash700 years Over 6 intense storms in the last 700 years41.3797°N -71.5211°W
French PolynesiaOverwash deposits5,000Increased activity between 5,000 – 3,800 and 2,900 – 500 years ago with relative inactivity since-16.6308°N -151.562°W
Thatchpoint BlueholeSedimentsAD 1010–presentRecorded storms include Hurricane Jeanne in 2004; active periods between 1050 and 1150 AD, a very active period between 1350-1650AD, a reincrease in the late 18th century26.3235°N -94.59°W
Coral blocks moved by storms1,100Increased storminess 1,100, 750, 600 and 350 years ago; correlated with storminess in French Polynesia and a recurrence rate of about 100–150 years -8.5333°N 184°W
Tzabnah CaveYucatanOxygen isotope ratios in stalagmitesAD 750 and earlierLow tropical cyclone activity at the time of the Classical Maya collapse, and more generally coinciding with drought20.75°N -117°W
Valdosta State UniversityOxygen isotope ratios in tree rings AD 1770 – 1990Historical storms have been recorded, as well as a trio in 1911–1913 and a strong event in 178030.8489°N -83.2892°W
Beach ridges 4,100 Strong storms (category 5) occur every 180 years
Walsingham CavernBermudaSediments in submarine cave3,100Increased storm activity between 3,000 – 1,700 and 600 – 150 years ago; however this record might include extratropical storms32.3333°N -104°W
Wassaw IslandGeorgiaOverwash1,900At least eight deposits from strong hurricanes between 1,000 – 2,000 years ago, with a quiet period between 1,100 and 250 years ago31.9055°N -80.9969°W
Florida, northwestern Overwash deposits7,000Between 3,800 – 1,000 years ago strike probability was about 0.5% per year, followed and preceded by relative inactivity [6] 30.3253°N -86.1533°W
Whale BeachSand sheets in marshesAD 1300–presentTwo major hurricanes in 700 years, one between 1278–1438 and the other is the 1821 Norfolk and Long Island hurricane39.1833°N -74.6714°W
Queensland, northern Beach ridges 4,500An inactive period between about 3,800 and 2,100 years ago was followed by an active on between 2,100 and 900 years ago-16.4231°N 145.4189°W
China, southernLagoonal sediments7,500Seven storm periods in the last 7,500 years, including active periods between 5,500 and 3,500 and from 1,700 years ago onwards, with inactive period in between; there are also (in)active periods embedded within these active(inactive) ones and there is more generally a correlation to storm activity elsewhere in southern China and to ENSO variations18.4167°N 110°W
Yok Balum Cave Oxygen isotope ratios in speleothemsAD 1550 – 1983 After an inactive phase (~1 storm/year) in the middle 16th century, an increase to ~8 storms/year in the 17th century associated with the Little Ice Age. Then a steady decrease until 1870, when occurrence halved and dropped to ~2 storms/year16.2086°N -89.0735°W
Yongshu ReefCoral blocks relocated by storms 4,000Six strikes in 1,000 years, with two during the Little Ice Age and four during the Medieval Climate Anomaly. Also high storm activity around 1200 AD, 400 BC and 1200 BC9.6167°N 170°W
Zhejiang-Fujian mud belt East China SeaMarine sediment cores2,000Increased activity between 0–480 CE, 790–1230 CE, and 1940–2018 CE28.69°N 122.41°W

Non-tropical examples

Place Country/state Data sources Record duration in years before present Conclusions Sources Approximate coordinates
France High-energy sedimentation8,000Between around 5720–5520 BC and 5050 BC–AD 360, storm activity was less meaningful. Increased storminess occurred AD 1350–1450, 150 BC–year 0, 900–400 BC, 1550–1320 BC, 3450–3420 BC, and 4700–4560 BC.46.7089°N -2.3596°W
France Overwash deposits1,500 Four intense storms in the last 1,500 years 43.53°N 3.9°W

See also

References

General sources

Further reading

External links

Notes and References

  1. Kiage . Lawrence M . A 1200-year history of environmental changes in Bay Jimmy area, coastal Louisiana, USA . The Holocene . 1 February 2020 . 30 . 2 . 201–209 . 10.1177/0959683619875801 . 2020Holoc..30..201K . en . 0959-6836. free .
  2. Brill . Dominik . Seeger . Katharina . Pint . Anna . Reize . Felix . Hlaing . Kay Thwe . Seeliger . Martin . Opitz . Stephan . Win . Khin Mi Mi . Nyunt . Win Thuzar . Aye . Nilar . Aung . Aung . Kyaw . Kyaw . Kraas . Frauke . Brückner . Helmut . Modern and historical tropical cyclone and tsunami deposits at the coast of Myanmar: Implications for their identification and preservation in the geological record . Sedimentology . April 2020 . 67 . 3 . 1431–1459 . 10.1111/sed.12586. 134771900 .
  3. May. Simon Matthias. Brill. Dominik. Leopold. Matthias. Callow. Nik. Engel. Max. Opitz. Stephan. Scheffers. Anja. Brückner. Helmut. 2017-04-01. 2017a. Washover fans in the Exmouth Gulf (NW Australia) – chronostratigraphical and geomorphological investigations and palaeotempestological significance. EGU General Assembly Conference Abstracts. 19. 16981. 2017EGUGA..1916981M.
  4. Liu . Kam-biu . Lu . Houyuan . Shen . Caiming . A 1200-year proxy record of hurricanes and fires from the Gulf of Mexico coast: Testing the hypothesis of hurricane–fire interactions . Quaternary Research . January 2008 . 69 . 1 . 30 . 10.1016/j.yqres.2007.10.011 . 2008QuRes..69...29L . 44126539 .
  5. Jeon . Byunggwon . Scircle . Austin . Cizdziel . James V. . Chen . Jingjing . Black . Oscar . Wallace . Davin J. . Zhou . Ying . Lepak . Ryan F. . Hurley . James P. . Historical deposition of trace metals in a marine sapropel from Mangrove Lake, Bermuda with emphasis on mercury, lead, and their isotopic composition . Journal of Soils and Sediments . 1 April 2020 . 20 . 4 . 2266–2276 . 10.1007/s11368-020-02567-6 . 210938630 . en . 1614-7480.
  6. Liu . Kam-biu . Fearn . Miriam L. . Reconstruction of Prehistoric Landfall Frequencies of Catastrophic Hurricanes in Northwestern Florida from Lake Sediment Records . Quaternary Research . September 2000 . 54 . 2 . 238. 10.1006/qres.2000.2166 . 2000QuRes..54..238L . 140723229 .