<%BANNER%>

UFIR



Spatial characteristics of tropical cyclone rainfall patterns in Florida
CITATION PDF VIEWER
Full Citation
STANDARD VIEW MARC VIEW
Permanent Link: http://ufdc.ufl.edu/IR00001370/00001
 Material Information
Title: Spatial characteristics of tropical cyclone rainfall patterns in Florida
Series Title: The Florida Geographer, 37, 58-71
Physical Description: Journal Article
Creator: Matyas, Corene
Publisher: The Florida Geographer
Publication Date: 2006
 Notes
Acquisition: Collected for University of Florida's Institutional Repository by the UFIR Self-Submittal tool. Submitted by Corene Matyas.
Publication Status: Published
 Record Information
Source Institution: University of Florida Institutional Repository
Holding Location: University of Florida
Rights Management: All rights reserved by the submitter.
System ID: IR00001370:00001

Downloads

This item is only available as the following downloads:

Matyas2006FlGeogProof ( PDF )


Full Text

PAGE 1

58 Florida Tropical Cyclone Rainfall Totals as Related to Storm Location and Intensity Corene Matyas Assistant Professor Department of Geography University of Florida Introduction As recently witnessed during the 2004 and 2005 Atlantic Basin hurricane seasons, Florida is highly susceptible to the effects of tropical cyclones (TCs). Its elongated shape an d location within the subtropics means that TCs forming in the Gulf of Mexico, Caribbean Sea, and the Atlantic Ocean can affect Florida (Vega and Binkley 1993). According to the National Hurri cane Center’s best track data, 475 named TCs have formed during th e past 48 Atlantic Basin hurricane seasons. Forty percent of th e 164 TCs that have made a U.S. landfall have come ashore over Florid a, which is more than any other state. When calculating return peri ods for hurricane landfalls in all U.S. coastal counties, Elsner a nd Kara (1999) found that Monroe County, Florida, experiences the high est frequency of hurricane landfalls, with a return period of four years. Dade and Broward counties have return periods of five years. These facts suggest that Florida is more subject to a direct hurricane strike than any other state along the U.S. Gulf of Mexico or East Coast. TCs can cause damage through fast winds, storm surge, tornadoes, and heavy rainfall. Although fa st winds and storm surge are of concern during a direct hurricane strike, Rappaport (2000) found that nearly 60% of U.S. TC-related deaths during 19701999 were due to fresh water flooding. Depending upon th e forward speed of the storm (Corbosiero and Mo linari 2003), moisture ava ilability (Chan et al. 2004), and interactions with the at mosphere and land surface (Gilbert and LaSeur 1957), heavy rainfall from TCs can commence prior to the circulation center’s la ndfall, continue for days after the storm has Florida Tropical Cyclone Rainfall Totals Matyas

PAGE 2

The Florida Geographer 59 tracked inland, and can even occu r when a TC does not make landfall. Thus, the effects of TC rain fall can be more widespread than those from fast winds and storm su rge. A ranking of the top ten TC rainfall totals for Atlantic Basin storms in the U.S. since 1980 shows that Florida experienced three of th ese ten high rainfall totals (Table 1). Three additional TCs on this li st tracked through Florida even though they produced their highest rain fall total in othe r states. Thus, in addition to a high risk of a dir ect hurricane strike, Florida is also vulnerable to high rainfall amounts produced by TCs that may or may not make landfall within the state. This study examines TC rainfa ll totals produc ed in Florida during the 1980-2005 Atlantic Basin hurricane seasons, and their relationship to the position of the stor m. Distances between the location of maximum Florida rainfall (LMFR) for each TC and the landfall of each TC are discussed to demonstrat e that TCs do not have to make landfall in Florida to produce heavy ra infall within the state, and to determine the distance over which a TC can travel from landfall and Rank Highest Rainfall (mm) Tropical Cyclone (Year) State of Landfall State Receiving Highest Rainfall Florida Storm Track a Maximum Florida Rainfall (mm) 1 1034 Allison (2001) TX, LA TX N 257 2 978 Georges (1998) MS FL Y 978 3 932 Danny (1997) LA, AL AL Y 178 4 711 Alberto (1994) FL GA Y 508 5 653 Allison (1989) TX LA N 127 6 650 Dennis (1981) FL, NC FL Y 650 7 612 Floyd (1999) NC NC N 76 8 599 Frances (2004) FL, FL NC Y 381 9 569 Frances (1998) TX LA N 0 10 546 Bob (1985) FL, SC FL Y 546 Table 1: Top Ten Rainfall Amount s Produced within the U.S. by Named Atlantic Basin Tropic al Cyclones during 1980-2005 a Y (N) indicates that the TC’s circulation center did (not) pass over Florida Data complied from the Hydrometeorological Prediction Center

PAGE 3

60 still produce rainfall within Florid a. To examine the spatial distribution of heavy rainfall amounts around the storm’s track, the distance between the LMFR and the location along the storm’s track that is closest to the LMFR is measured to determine whether locations close to the storm track receive the highest rainfall totals. Several physical forcing mechanisms that affect TC rainfall production are discussed to explain variations in TC rainfall patterns over Florida. Data and Methods A list of the highest storm total rainfall amount produced by each U.S. landfalling TC and the location receiving this rainfall is available from the Hydrometeorol ogical Prediction Center website (http://www.hpc.ncep.noaa.gov/tropical /rain/tcmaxima.html). This information was utilized to create Table 1 and identify which TCs produced their highest rainfall totals in Florida. Selected rainfall totals reported in the National Hurricane Center (NHC)’s best track dataset, or rainfall totals listed in the storm summary for TCs where individual observations were not lis ted, were utilized to determine the rainfall amounts received in Florida for all other TCs in the current study. Although these data are the official storm total rainfall amounts recorded by rain gauges at each station, it should be noted that these data may underestimate the actual rainfall amounts that occurred with each storm (Nystuen 1999). A Geographic Information System (GIS) was utilized to calculate the distance between the LM FR and the landfall location, and between the closest point along the storm track to the LMFR and the LMFR. Storm track coordinates were obtained from the National Oceanic and Atmospheric Administra tion Coastal Services Division, where storm track data have been converted into a GIS-compatible format (http://hurricane.csc.no aa.gov/hurricanes/download.html). Data utilized to determine the inte nsity of the storm when the TC was closest to Florida are also contained within this dataset. Results Of the 335 TCs that formed w ithin the Atlantic Basin during 1980-2005, 71 (61) produced at leas t 25.4 mm (125 mm) of rainfall Florida Tropical Cyclone Rainfall Totals Matyas

PAGE 4

The Florida Geographer 61 within Florida. Forty Atlantic Ba sin TCs produced their highest rainfall amounts within Florida, nearly twice the amount of Texas, which had the second highest number of TC rainfall maxima during this period. These figures demonstrate that in addition to the effects of fast winds and storm surge associated w ith a direct landfall, Florida is also susceptible to the effects of TC rainfa ll, which can occur without a direct landfall. The average rainfall maximum for the 71 TCs producing 25.4 mm or greater rainfall totals wa s 270 mm (10.6 in) (Figure 1). Six TCs produced over 500 mm (20 in) of rainfall, and these rainfall amounts occurred within 75 km of th e TC’s circulation center (Table 2), suggesting that TCs produce their highest rainfall totals close to the storm’s center. However, not all of these rainfall totals were produced near the point of landfall. Hurricane Georges (1998) made landfall over 200 km from its LMFR demonstrating that TCs making landfall in other states can still pr oduce heavy rainfall within Florida. Figure 1: Maximum Rainfall Am ounts Produced by Tropical Cyclones in Florida 1980-2005

PAGE 5

62 The following two sections discuss the landfall locations of TCs producing rainfall in Florida, and the distribution of the LMFR about the storm track to ascertain the range of distances over which TC rainfall has affected Florida. Distance from Landfall Point It is important to determine the distance over which a TC can travel from its landfall point to produce heavy rainfall within Florida so that people will remain aware of conditions even after landfall has occurred. Most (70% of) TCs tend to produce their highest rainfall amounts in Florida when they make landfall within 50 km (300 km) Florida Tropical Cyclone Rainfall Totals Matyas Table 2: Top Ten Maximum Rainfall Amounts Produced by Tropical Cyclones in Florida 1980-2005 Ran k Max. Rain (mm) Tropical Cyclone (year) Int. a LMFR b Distance to track (km) c Distance from landfall (km) 1 978 Georges (1998) TD Munson 5 R, L 225 2 650 Dennis (1981) TS Homestead 65 R 65 3 635 TD # 1 (1992) TD Arcadia Tower 75 R 75 4 546 Bob (1985) TS Everglades City 40 R 55 5 508 Alberto (1994) TS Niceville 15 R, L 10 6 508 Erin (1995) H DeFuniak Springs 0 0 7 445 Leslie (2000) TD South Miami 255 R No landfall 8 443 Irene (1999) H Boynton Beach 75 R 210 9 427 Jerry (1995) TS Golden Gate 140 L 210 10 419 Alberto (1982) TD Tavernier 225 R No landfall a Int is the intensity of the TC when it affected Florida b Location of Maximum Florida Rainfall c Distance to track includes whether the gauge was located to the left (L) or right (R) of the storm track

PAGE 6

The Florida Geographer 63 of the LMFR (Figure 2). Howeve r, as witnessed during Tropical Storm Allison (2001), heavy rainfall can also occur in Florida up to 1050 km from the point of landfa ll (Figure 1). Jefferson County, Texas received 1033 mm (40.68 in) of ra infall in total, the highest amount produced by a TC in the U.S. during 1980-2005 (Table 1). Six days after the initial landfall over Freeport, Texas, Allison produced 257 mm of rainfall over Talla hassee, Florida. Subtropical ridges located on either side of Alli son were responsible for its slow forward velocity and eventual north east track. Over half of the 41 deaths caused by Allison were due to fresh water flooding; eight people died in Florida (Beven et al. 2003). This example illustrates that Florida residents need to exercise caution even after a TC has made landfall and even though landfall may occur several states away. The highest amount of rainfall within Florida during 19802005 occurred with Hurricane Georges (1998) (Table 2). Like Allison, Georges did not make landfall within Florida. However, the cirFigure 2: Distance Between the Landfall Location and the Florida City Receiving the Maximum Rainfall Amount

PAGE 7

64 culation center of Georges did pa ss through northern Florida the day following its landfall near Biloxi Mississippi (Pasch, Avila, and Guiney 2001). Munson, Florida, lo cated 225 km east from Biloxi, Florida Tropical Cyclone Rainfall Totals Matyas Figure 3: Tracks for Tropical Cyclones Producing Over 75 mm of Rainfall in Florida during: a) 1980-1985, b) 1986-1990, c) 19911995, d) 1996-2000, e) 2001-2005, f) legend a b c d e f

PAGE 8

The Florida Geographer 65 received 978 mm (38.46 in) of rainfa ll from Georges. Several rain gauges approximately 75 km west of Munson and 150 km east from Biloxi, recorded rainfall totals between 635-765 mm, indicating that Georges produced heavy rainfall in multiple locations. Even though Georges made landfall as a Category 2 hurricane on the SaffirSimpson scale (Simpson and Rhiel 1981), the effects of its heavy rainfall were much more wide-spread than from its fast winds, as hurricane-force winds only extended an average of 51 km outward from its circulation center. Allison and Georges are two ex amples of TCs that produced heavy rainfall within the state of Florida, although neither storm made landfall within the state. The second highest total rainfall amount for Florida since 1980 was produced by Tropical Storm Dennis (1981) (Table 2), a storm that did make landfall in Florida (Lawrence and Pelissier 1982). Home stead received 390 mm of rainfall within 24 hours as Dennis made landfall in Monroe County and tracked north, entering the Atlantic Ocean near Daytona Beach. The LMFR for Dennis occurred 65 km fr om its point of landfall. Lawrence and Pelissier (1982) estimated that over $25 million in damage was caused by the rainfall of De nnis in southern Florida. As a TC making landfall over 1000 km west of Florida can still produce heavy rainfall within th e state, it is important to determine which features of the atmosphe re influence TC tracks. Plotting storm tracks for TCs that have produced rainfall within Florida illustrates several different trajectories taken by th ese 65 TCs (Figure 3). Large-scale circulation patterns usua lly determine the track of a particular TC (Wu and Wang 2004). Varia tions in the storm tracks of North Atlantic Basin TCs can be attr ibuted to the positions of the polar jet stream over North America and the subtropical high in the North Atlantic Ocean (Elsner, Liu, and Kocher 2000). Both the atmosphere and the land surface can affect a TC’s track. When experiencing high wind shear, Ueno (2003) found that the differing wind speeds and direc tions throughout th e vertical column of the troposphere can cause a variety of TC tracks. Modeling work by Dengler (1997) showed that the orientation of the coastline could deflect the track of a landfal ling TC. In the absence of these

PAGE 9

66 features, the storm’s inertia carries it towards the northwest in the northern hemisphere. Given the comp lex interactions between a TC and its environment, Florida resi dents must exercise caution throughout the hurricane season, and prepare for the possibility that a storm making landfall in Texas could move eastward and produce heavy rainfall in northern Florida, or th at a TC moving th rough the Florida Straights may not make landfall, but could still produce heavy rainfall in the southern portion of the state. Position of Maximum Florida Rainfall Relative to the Storm Track The TCs examined in this study produced their Florida rainfall maxima at distances ranging from the storm’s circulation center out to 610 km from the circulation ce nter (Figure 4). More than half (40 percent) of the LMFRs were le ss than 100 km (50 km) from the storm track, suggesting that locations closer to the storm track are more likely to experience high rainfall totals. The side of the storm track where the LMFR occurred was also examined. The LMFR occurred on the left side of the storm track in 34 percent of the cases examined, while 18 percent of TC s produced rainfall maxima on both sides of the storm track. To better understand how rainfall can be produced ahead of and/or to either side of the storm track at varying distances, it is important to understa nd the physical forcing mechanisms that control rainfall production with the TC. The movement of winds from the re latively smooth ocean surface to the rougher land surface can also enhance rainfall production in certain portions of the storm. The onshor e winds converge as they slow, which enhances uplift and precipita tion generation (Parrish et al. 1982). In a TC making landfall at a pe rpendicular angle to a straight coastline, this enhanced uplift occurs on the right side of the storm in the northern hemisphere. Rogers a nd Davis (1993) demonstrated that the shape and orientation of the co astline can affect where this enhanced rainfall is produced within the storm. Faster tangential winds and/or a smaller radius of maximu m winds would allow moisture to circulate about the storm before precipitating out (Li et al. 1997), which could produce a rainfall maximum on the left side of the storm. Due to the relatively narrow shape of Florida’s peninsula, it is possi-Florida Tropical Cyclone Rainfall Totals Matyas

PAGE 10

The Florida Geographer 67 ble for onshore winds to occur on the coastline opposite from where the storm center makes landfall. Th erefore, a TC making landfall on the west coast of Florida could produce a rainfall maximum on the east coast of Florida on the left side of the storm. This process could also account for increased rainfall amounts to the left of the storm track. TC interactions with the atmo sphere can also cause a TC’s rain shield to become displaced from the circulation center of the storm. For example, strong vertical wind shear inhibits rainfall from occurring on the upshear side of the storm (Corbosiero and Molinari 2003). In other words, if the wind shear is from the west, most rainfall will occur on the east side of the storm. If a storm experiencing westerly wind shear is moving towards the east, the rain shield will be displaced ahead of the storm, a nd locations on either side of the storm track could experience hea vy precipitation. Strong wind shear Figure 4: Distance of Location of Florida Rainfall Maximum from the Closest Approach of the Tropical Cyclone’s Circulation Center

PAGE 11

68 causing a displaced rain shield could account for the large distances between some LMFRs and the TC circulation centers. As stated previously, the majo rity of LMFRs occurred within 100 km of the storm track. Pearson correlation coefficients were calculated to determine if a relationshi p existed between the rainfall total and the proximity of the storm track for the 69 TCs producing at least 75 mm of rainfall (Table 3). All TCs were analyzed together and then were stratified by intensity. The storm’s intensity was defined using its maximum sustained wind speed when first entering or at its nearest position to Florida. Results suggest that hurricanes produce higher storm total rainfall amounts close to their stor m track. Marks et al. (2002) found through an examination of 245 TCs that high rain rates for hurricanes were located closer to the storm cen ter than for tropical storms, which supports the correlation coefficients calculated in th e current study. In the Marks et al. (2002) study, peak hurricane rainfall rates exceeded 7 mm/hr at a distance 25 – 50 km away from the storm center. Rainfall rates decreased to 4 mm/hr 125-150 km away from the storm center, and 1 mm/hr 250-300 km away from st orm center. This decrease in rain rates away from the storm cen ter would correspond to decreasing rainfall totals away from the storm center. Conclusions and Future Research This study examined the location receiving the maximum storm total rainfall amount within Florida for TCs that occurred during 1980-2005. Seventy-one TCs produced an inch or more of rainfall within Florida during this period, w ith an average maximum rainfall Florida Tropical Cyclone Rainfall Totals Matyas Table 3: Correlation Values for Maximum Rainfall Amounts and the Distance from the Storm Track at which they Occurred Type All Data Hurricanes Tropical Storms Tropical Correlation -0.42* -0.72* -0.36 -0.34 No. Cases 69 19 29 21 denotes significance at the 0.01 level

PAGE 12

The Florida Geographer 69 total of 254 mm (10.6 in). The loca tions of these Florida rainfall maxima were compared to the landfall location of each TC, and the TC’s closest position to the point of rainfall maxima to determine the range of distances over which Florid a residents should be on alert for the potential of TC-produced rainfall. TCs making landfall as far away as Texas have tracked eastwar d to produce rainfall in Florida, and six TCs affected Florida with out making a U.S. landfall. This finding suggests that people in Flor ida should prepare for the possibility of TC-produced rainfall even when a TC is forecast to come ashore in other states. More than half of the TCs ex amined produced their Florida maximum rainfall within 100 km of either side of the storm track. Yet, 20 percent of the LMFR were located more than 300 km from the storm track, suggesting that Flor ida residents need to stay informed about potential rainfall haza rds even if the TC is not forecast to track directly thr ough their area. Although intensity does not appear to influence the maximum amount of rainfall received, an inverse relationship was found between hurricane rainfall totals and distance from the storm track. The key factors proposed by this study to enhance rainfall for storms tr acking through Florida are interactions with the atmosphere which a ffect the speed of motion and moisture availability, and frictional convergence al ong the coastline. Future research will further investigate the atmospheric and land surface physical forcing mechanisms responsible for TC rainfall production in Florida. TCs whose tracks were influenced by similar atmospheric conditions will be grouped to identify similarities in rainfall patterns resulting from atmospheric physical forcing mechanisms. TCs making landfall along coas tlines of similar shape, and TCs of similar intensity and radius of maximum winds will be examined together to determine the effects of enhanced friction and convergence at the coastline. Acquisition of data for all Florida stations receiving rainfall for each TC will f acilitate a calculation of the area over each TC produces rainfall, and the amount of TC-produced rainfall received each year.

PAGE 13

70 References Beven, J. L., S. R. Stewart, M. B. Lawrence, L. A. Avila, J. L. Franklin, and R. J. Pasch. 2003. Annua l summary: Atlantic hurricane season of 2001. Monthly Weather Review 131 (7):14541484. Chan, J. C. L., K. S. Liu, S. E. Ching, and E. S. T. Lai. 2004. Asymmetric distribution of convecti on associated with tropical cyclones making landfall along the south China coast. Monthly Weather Review 132 (10):2410-2420. Corbosiero, K. L., and J. Molin ari. 2003. The relationship between storm motion, vertical wind sh ear, and convective asymmetries in tropical cyclones. Journal of the Atmospheric Sciences 60 (2):366-376. Dengler, K. 1997. A numerical study of the effects of land proximity and changes in sea surface temperature on hurricane tracks. Quarterly Journal of the Ro yal Meteorological Society 123 (541):1307-1321. Elsner, J. B., and A. B. Kara. 1999. Hurricanes of the North Atlantic New York: Oxford University Press. Elsner, J. B., K. B. Liu, and B. Kocher. 2000. Spatial variations in major US hurricane activity: Statistics and a physical mechanism. Journal of Climate 13 (13):2293-2305. Gilbert, S. C., and N. E. LaSeur. 1957. A study of the ra infall patterns and some related features in a dissipating hurricane. Journal of Meteorology 14:18-27. Lawrence, M. B., and J. M. Pelis sier. 1982. Atlantic hurricane season of 1981. Monthly Weather Review 110 (7):852-866. Li, J. J., N. E. Davidson, G. D. Hess, and G. Mills. 1997. A highresolution prediction study of two typhoons at landfall. Monthly Weather Review 125 (11):2856-2878. Marks, F. D., G. Kappler, and M. DeMaria. 2002. Development of a tropical cyclone rainfall climatology and persistence (RCLIPER) model. Paper read at 25th Conference on Hurricanes and Tropical Meteorology, Americ an Meteorological Society, at San Diego, CA. Florida Tropical Cyclone Rainfall Totals Matyas

PAGE 14

The Florida Geographer 71 Nystuen, J. A. 1999. Relative perfor mance of automatic rain gauges under different rainfall conditions. Journal of Atmospheric and Oceanic Technology 16 (8):1025-1043. Parrish, J. R., R. W. Burpee, F. D. Marks, and R. Grebe. 1982. Rainfall patterns observed by digitized radar dur ing the landfall of Hurricane Frederic (1979). Monthly Weather Review 110 (12):1933-1944. Pasch, R. J., L. A. Avila, and J. L. Guiney. 2001. Atlantic hurricane season of 1998. Monthly Weather Review 129 (12):30853123. Rappaport, E. N. 2000. Loss of life in the United States associated with recent Atlantic tropical cyclones. Bulletin of the American Meteorological Society 81 (9):2065-2073. Rogers, R. F., and R. E. Davis. 1993. The effect of coastline curvature on the weakening of Atlantic tropical cyclones. International Journal of Climatology 13 (3):287-299. Simpson, R. H., and H. Rhiel. 1981. The Hurricane and Its Impact Baton Rouge: Louisiana State University Press. Ueno, M. 2003. Steering weight concep t and its application to tropical cyclones simulated in a vertical shear experiment. Journal of the Meteorologica l Society of Japan 81 (5):1137-1161. Vega, A. J., and M. S. Binkley. 1993. Tropical cyclone formation in the North Atlantic basin, 1960-1989. Climate Research 3:221232. Wu, L. G., and B. Wang. 2004. Asse ssing impacts of global warming on tropical cyclone tracks. Journal of Climate 17 (8):16861698.