Meteorological Causes of the Secular Variations in Observed Extreme Precipitation Events for the Conterminous United States

AbstractDaily extreme precipitation events, exceeding a threshold for a 1-in-5-yr occurrence, were identified from a network of 935 Cooperative Observer stations for the period of 1908–2009. Each event was assigned a meteorological cause, categorized as extratropical cyclone near a front (FRT), extratropical cyclone near center of low (ETC), tropical cyclone (TC), mesoscale convective system (MCS), air mass (isolated) convection (AMC), North American monsoon (NAM), and upslope flow (USF). The percentage of events ascribed to each cause were 54% for FRT, 24% for ETC, 13% for TC, 5% for MCS, 3% for NAM, 1% for AMC, and 0.1% for USF. On a national scale, there are upward trends in events associated with fronts and tropical cyclones, but no trends for other meteorological causes. On a regional scale, statistically significant upward trends in the frontal category are found in five of the nine regions. For ETCs, there are statistically significant upward trends in the Northeast and east north central. For the ...

[1]  Mesoscale Convective Complexes Over the United States During 1981— Annual Summary , 1982 .

[2]  Jeffrey S. Whitaker,et al.  Feasibility of a 100-Year Reanalysis Using Only Surface Pressure Data , 2006 .

[3]  David B. Knight,et al.  Contribution of tropical cyclones to extreme rainfall events in the southeastern United States , 2009 .

[4]  R. Arritt,et al.  Mesoscale Convective Systems over the United States during the 1997–98 El Niño , 2001 .

[5]  David R. Easterling,et al.  Quality Control of Pre-1948 Cooperative Observer Network Data , 2005 .

[6]  Xue Wei,et al.  Reanalysis without Radiosondes Using Ensemble Data Assimilation , 2004 .

[7]  D. Easterling,et al.  Recent increases in U.S. heavy precipitation associated with tropical cyclones , 2010 .

[8]  D. M. Rodgers,et al.  Mesoscale Convective Complexes over the United States during 1983 , 1985 .

[9]  K. Howard,et al.  Mesoscale convective complexes over the United States during 1982 , 1983 .

[10]  David R. Easterling,et al.  Contemporary Changes of the Hydrological Cycle over the Contiguous United States: Trends Derived from In Situ Observations , 2004 .

[11]  Christopher J. Anderson,et al.  Mesoscale Convective Complexes and Persistent Elongated Convective Systems over the United States during 1992 and 1993 , 1998 .

[12]  Kenneth W. Howard,et al.  Mesoscale Convective Complexes over the United States during 1985 , 1988 .

[13]  D. Easterling,et al.  A Monte Carlo Assessment of Uncertainties in Heavy Precipitation Frequency Variations , 2007 .

[14]  R. Reynolds,et al.  The NCEP/NCAR 40-Year Reanalysis Project , 1996, Renewable Energy.

[15]  Thomas R. Karl,et al.  Secular Trends of Precipitation Amount, Frequency, and Intensity in the United States , 1998 .

[16]  D. Easterling,et al.  Temporal variations of extreme precipitation events in the United States: 1895–2000 , 2003 .

[17]  P. Jones,et al.  The Twentieth Century Reanalysis Project , 2009 .

[18]  C. J. Neumann Tropical cyclones of the North Atlantic Ocean, 1871-1986. , 1987 .

[19]  D. Easterling,et al.  Trends in Intense Precipitation in the Climate Record , 2005 .

[20]  K. Howard,et al.  Mesoscale Convective Complexes over the United States during 1986 and 1987 , 1991 .