United States tropical cyclone rainfall climatology

From Wikipedia, the free encyclopedia
Jump to: navigation, search
All tropical cyclone tracks between the years 1985 and 2005.

The United States tropical cyclone rainfall climatology concerns the amount of precipitation, primarily in the form of rain, which occurs during tropical cyclones and their extratropical cyclone remnants across the United States. Typically, five tropical cyclones and their remnants impact the country each year, contributing between a tenth and a quarter of the annual rainfall across the southern tier of the country. The highest rainfall amounts appear close to the coast, with lesser amounts falling farther inland. Obstructions to the precipitation pattern, such as the Appalachian mountains, focus higher amounts from northern Georgia through New England. While most impacts occur with systems moving in from the Atlantic ocean or Gulf of Mexico, some emanate from the eastern Pacific ocean, with a few crossing Mexico before impacting the Southwest. Those making landfall within the Southeast portion of the country tend to have the greatest potential for heavy rains.

Long-term averages[edit]

On average, five North Atlantic hurricanes or their remnants lead to rainfall across the contiguous United States each year, contributing between a tenth and a quarter of the annual rainfall to the southern United States. While many of these storms form in the Atlantic Basin, some systems or their remnants move through Mexico from the Eastern Pacific Basin. Tropical cyclones from the eastern Pacific bring nearly 20 percent of the average annual rainfall to southern California.[1] The average storm total rainfall for a tropical cyclone impacting the lower 48 from the Atlantic Basin is about 16 inches/406 mm, with 70-75 percent of the storm total falling within a 24‑hour period.

Highest known amounts for the lower 48 since 1962[edit]

Below is a list of the top ten highest known storm total rainfall amounts from individual tropical cyclones across the lower 48 since 1962. Four of the wettest systems struck Texas, two strongly impacted Louisiana, while one each made their biggest mark on Mississippi, Georgia, Virginia, and Florida.

  1. 1219 mm/48.00 inches Amelia 1978
  2. 1143 mm/45.00 inches Claudette 1979
  3. 1033 mm/40.68 inches Allison 2001
  4. 977 mm / 38.46 inches Georges 1998
  5. 932 mm / 36.71 inches Danny 1997
  6. 707 mm / 27.85 inches Alberto 1994
  7. 695 mm / 27.38 inches Beulah 1967
  8. 686 mm / 27.00 inches Camille 1969
  9. 652 mm / 25.67 inches Allison 1989
  10. 649 mm / 25.56 inches Dennis 1981[2]

Maximum per state for the Lower 48[edit]

U.S. tropical cyclone rainfall maxima per state

State maxima relating to tropical cyclones and their remnants are shown on the left, color-coded by amount. Tropical cyclones from the Atlantic Basin have the most sway along the Gulf coast and Eastern Seaboard. The impact of tropical cyclones and their remnants originally from the eastern Pacific stretches as far east as Michigan and Indiana. Rainfall related to the low pressure area once associated with a tropical cyclone, or its remnants aloft, are included in this sample. No additional rainfall from pre-existing upper lows as seen before cyclones such as Hurricane Fran of 1996 or from upper cyclones that closed off behind former tropical cyclones such as Hurricane Juan of 1985 was included.[3]

The state of Texas has the highest amounts, followed by Florida, Alabama, and Mississippi. Out West, the same can be said for Hurricane Kathleen (1976) and the remains of Hurricane Olivia of the 1982 Pacific hurricane season. Some records across the Midwest occurred during Tropical Storm Candy of 1968.[3]

U.S. Tropical Cyclone Rainfall Accumulations per time frame

Average and record statistics per time frame for the lower 48[edit]

To the right is a graphic showing averages and extremes for a 15-year sample of tropical cyclones and their remnants affecting the contiguous United States. The units of the rainfall amounts are in inches, while the time units are in hours. The bars in the graph express the percent of the storm total rainfall, which is defined to be 100 percent in the final column. Note that, on average, as much as one-fourth of the total occurs in 2–3 hours, while half falls within 12 hours, and almost three-quarters of the storm total falls within a 24‑hour period. Cases where a cyclone scraped the coast were not separated out from those that made a more direct landfall. Also, Pacific and Atlantic cases were not separated. This all explains the average storm total of the sample being depressed to 338.8 mm/13.34". On the bottom of the graphic are listed the averages per time frame and the records. The records were mainly set during Tropical Storm Allison (2001) and Hurricane Danny (1997). This graphic will be updated as the climatology pushes farther back in time.[4]

United States rules of thumb for forecasting[edit]

Kraft rule[edit]

During the late 1950s, this rule of thumb came into being, developed by R. H. Kraft.[5] It was noted from rainfall amounts (in imperial units) reported by the first order rainfall network in the United States that the storm total rainfall fit a simple equation: 100 divided by the speed of motion in knots.[6] This rule works as long as a tropical cyclone is moving and only the first order or synoptic station network (with observations spaced about 60 miles/100 km apart) are used to derive storm totals. Canada uses a modified version of the Kraft rule which divides the results by a factor of two, which takes into account the lower sea surface temperatures seen around Atlantic Canada and the prevalence of systems undergoing vertical wind shear at their northerly latitudes.[7] The main problem with this rule is that the rainfall observing network is denser than either the synoptic reporting network or the first order station networks, which means the absolute maximum is likely to be underestimated. Another problem is that it does not take the size of the tropical cyclone or topography into account.

Eight inch or 203 mm rule[edit]

Rusty Pfost, now the head of the Miami National Weather Service Forecast Office, did a study in 1999 reviewing rainfall totals from tropical systems affecting Florida between 1960 and 1998. He found that for tropical cyclones moving at greater than 6 knots, the average storm total was normally in the 5–10 inch (127–254 mm) range. Slower moving storms usually forced greater than 15 inches (381 mm) of rain to fall.[6]

Sixteen inch or 406 mm rule[edit]

U.S. Tropical Cyclone Rainfall Accumulations per time frame

David Roth, a forecaster at the Hydrometeorological Prediction Center, determined that the average amount for all tropical cyclones impacting the United States was 13.34 inches (339 mm) between 1991 and 2005.[8] When removing the storms that grazed the domain, an average of near 16 inches/406 mm was obtained.[9] Using this latter amount appears to work best for systems that experience little vertical wind shear and are of at least average size. Amounts measured in small/midget tropical cyclones showed storm total amounts closer to 6 inches/152 mm. Operationally, variations to these amounts are introduced if the cyclone encounters mountain zones, interacts with a nearby front, or the storm is significantly sheared.[6]

See also[edit]


  1. ^ Kristen L. Corbosiero; Michael J. Dickinson & Lance F. Bosart. "The Contribution of Eastern North Pacific Tropical Cyclones to the Rainfall Climatology of the Southwest United States". Monthly Weather Review. American Meteorological Society. 137 (8): 2415–2435. Bibcode:2009MWRv..137.2415C. doi:10.1175/2009MWR2768.1. ISSN 0027-0644. 
  2. ^ Roth, David M. (April 29, 2015). "Tropical Cyclone Point Maxima". Tropical Cyclone Rainfall Data. United States Weather Prediction Center. Retrieved May 8, 2016. 
  3. ^ a b David M. Roth (2009-09-15). "Maximum Rainfall Caused By Tropical Cyclones and Their Remnants Per State (1961-2009)". Hydrometeorological Prediction Center. Retrieved 2010-01-21. 
  4. ^ Roth, David (2007-01-01). "Tropical Cyclone Rainfall Data". Hydrometeorological Prediction Center Home Page. National Weather Service. Retrieved 2007-01-13. 
  5. ^ Frank Marks. WSR-88D Derived Rainfall Distributions in Hurricane Danny (1997). Retrieved on 2007-04-13.
  6. ^ a b c Norman W. Junker. Hurricanes and Extreme Rainfall. Retrieved on 2007-03-15.
  7. ^ David M. Roth Tropical Cyclone Rainfall (July 2007 presentation). Retrieved on 2007-07-19.
  8. ^ David Roth. Tropical Cyclone QPF. Retrieved on 2007-03-15.
  9. ^ David Roth. Developing a Recent Tropical Cyclone Rainfall Climatology For the United States. 25th Conference on Hurricanes and Tropical Meteorology. American Meteorological Society, 2002.

External links[edit]