# Presentation: 011872

## Shift of Summer Precipitation Variability in the Southeast United States

- Hui Wang and Rong Fu, School of Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332-0340

- 	**1.  Introduction**
- 	The Southeast United States is one of the fastest growing regions in the nation.  Water supplies in this area are increasingly stressed especially during summer.  The year-to-year fluctuations in summer precipitation over the Southeast thus have vital influence on regional hydrology, agriculture, and related industries.  In the past three decades, summer droughts repeatedly struck the Southeast and had a devastating impact on this region both socially and economically.

- 	Figure 1 indicates that Southeast summer precipitation is an important part of warm season rainfall on the continental scale.

- 	**2.  Data**
- 	Precipitation:  U.S. Unified Precipitation for 1948–1998
- 	                        U.S. Daily Precipitation Analysis for 1999–2004
- 	                        0.25o lat × 0.25o long
- 	NCEP Reanalysis: 200-hPa and 850-hPa wind, 500-hPa height
- 	                              1948–2004
- 	SST:  Reconstructed Reynolds Data, 1948–2004

- 	**3. ****Variability of Southeast summer precipitation**

- Fig. 1

- Summer Mean Precipitation

- Precipitation Variance

- mm/day

- mm2/day2

- 	**Objectives**
- 	a. To determine whether the interannual anomalies of Southeast summer precipitation have become more variable and whether Southeast summer droughts and wetness have become more intense in the most recent three decades.
- 	b. To explore potential causes of the changes in the Southeast summer precipitation variability.

- Southeast US Summer Precipitation Index

- Wavelet Power Spectra

- 	The Southeast summer precipitation (Fig. 2) displays higher interannual variability with more wet and dry extremes in the second half of the period (1977–2004).

- Fig. 2

- 	Regression patterns of 200-hPa zonal wind anomalies associated with 1 mm/day rainfall deficit in the Southeast and variance of 200-hPa zonal wind.

- 1948–1975                    200-hPa Zonal Wind                      1977–2004

- Fig. 5

- 1948–1975                      Zonal Wind Variance                    1977–2004

- 5% significance
- level

- Summer Rainrate Distribution

- Fig. 3

- No rain               0.1 – 1                   1 – 10                   > 10  mm/day
-                                              Rainrate

- % of summer days

- 5 driest summers (1948-1975)         5 wettest summers (1948-1975)
- 5 driest summers (1977-2004)         5 wettest summers (1977-2004)
- 1948-2004 long-term mean

- 	Changes in both frequency and intensity of rainfall contribute to the higher precipitation variability after 1976 (Fig. 3).

- Precipitation Anomaly   1993

- Precipitation Anomaly   2000

- r( US Precip, SE Precip Index)

- Fig. 4

- mm/day

- 	Precipitation anomalies in the Southeast and the Midwest are out of phase (Fig. 4).

- 	**4. ****Relation to large-scale circulation**

- 1948–1975               500-hPa Height and Wave Activity Flux                1977–2004

- Fig. 6

- 	In both periods southeast summer drought is associated with positive height anomalies in the central and eastern United States and negative anomalies along the coasts of New England and the Pacific Northwest.  Over the North Pacific the relation to the circulation pattern is very different between the two periods.

- 	Southeast droughts are associated with an anticyclonic circulation over the central and eastern United States. The northeasterly flow off the Gulf coast suppresses moisture transport to the Southeast.

- 	**5. Summary**
- 	Southeast summer rainfall has exhibited higher interannual variability since around 1976, with a larger decrease (increase) of frequency and intensity of precipitation in dry (wet) summers.  It is suggested that a phase shift of the PDO in 1976 and higher SST variability after that may help enhance the variability of Southeast summer precipitation.

- 1977–2004

- 850-hPa Wind and SST Anomalies                     1948–1975

- Fig. 7

- SST Difference between
- (1977–2004) and (1948–1975)

- SST Variance
- 1948–1975

- 1977–2004

- 	A phase change of the PDO in 1976 reinforces the meridional SST gradient south of 40oN. North Pacific SST also exhibits higher variability after 1976.

- Fig. 8

- 	In the North Pacific large wind anomalies occur in regions between warm and cold SSTs, indicating a circulation response to the SST gradient.

**Variance:   30%           70%**

- 5% significance level

- 5% significance level

- 1976

- K

- K2

- 8
- 6
- 4
- 2
- 0

**Period (yr)**

**Year**