Global lightning activity from the ENSO perspective

[1] The recently reprocessed (1998–2006) OTD/LIS space-based lightning database is used to investigate the global lightning climatology in response to the ENSO cycle. Temporal correlation maps depicting lightning anomalies-NINO3.4 identify areas that generally follow patterns similar to the widely documented ENSO-related precipitation anomalies. However, areas having statistically significant lightning anomaly-NINO3.4 correlations accompanied by non-significant precipitation anomaly-NINO3.4 correlations are found over the mid-latitudes in both hemispheres. Analysis shows that these areas are related to upper level circulation anomalies (enhanced wind shear) induced by the corresponding ENSO phase. A special case is observed over the western Maritime continent where typical drought conditions during the warm ENSO phase are related to enhanced lightning activity. Further attention is given toward identifying areas over which consistent thunderstorm activity is observed during the two major warm and cold ENSO phases of the past decade. Their spatial distribution shows strong regional preference and in general agrees with the already established ENSO-related precipitation regimes.

[1]  E. Rasmusson,et al.  Meteorological Aspects of the El Ni�o/Southern Oscillation , 1983, Science.

[2]  C. Ropelewski,et al.  Global and Regional Scale Precipitation Patterns Associated with the El Niño/Southern Oscillation , 1987 .

[3]  J. Bjerknes ATMOSPHERIC TELECONNECTIONS FROM THE EQUATORIAL PACIFIC1 , 1969 .

[4]  Song Yang,et al.  Variations of the East Asian Jet Stream and Asian–Pacific–American Winter Climate Anomalies , 2002 .

[5]  Chunzai Wang ENSO, Atlantic Climate Variability, and the Walker and Hadley Circulations , 2004 .

[6]  W. Koshak,et al.  The Optical Transient Detector (OTD): Instrument Characteristics and Cross-Sensor Validation , 2000 .

[7]  J. Wallace,et al.  The Global Distribution of the Annual and Semiannual Cycles in Precipitation , 1976 .

[8]  P. Xie,et al.  Global Precipitation: A 17-Year Monthly Analysis Based on Gauge Observations, Satellite Estimates, and Numerical Model Outputs , 1997 .

[9]  H. Christian Global Frequency and Distribution of Lightning as Observed From Space , 2001 .

[10]  M. Mcphaden,et al.  Genesis and evolution of the 1997-98 El Nino , 1999, Science.

[11]  T. Delcroix,et al.  ENSO-Related Precipitation Changes in New Caledonia, Southwestern Tropical Pacific: 1969–98 , 2000 .

[12]  Chester F. Ropelewski,et al.  North American Precipitation and Temperature Patterns Associated with the El Niño/Southern Oscillation (ENSO) , 1986 .

[13]  E. Y. Hamid,et al.  Impact of the 1997–98 El Niño Event on lightning activity over Indonesia , 2001 .

[14]  E. Rasmusson,et al.  The Relationship Between Eastern Equatorial Pacific Sea Surface Temperatures and Rainfall over India and Sri Lanka , 1983 .

[15]  D. Enfield,et al.  Tropical Atlantic sea surface temperature variability and its relation to El Niño‐Southern Oscillation , 1997 .

[16]  Phillip A. Arkin,et al.  The Relationship Between Interannual Variability in the 200 mb Tropical Wind Field and the Southern Oscillation , 1982 .

[17]  Walter A. Petersen,et al.  Regional Variability in Tropical Convection: Observations from TRMM , 2001 .

[18]  Dennis E. Buechler,et al.  The 1997–98 El Nino event and related wintertime lightning variations in the southeastern United States , 2000 .

[19]  Ralf Toumi,et al.  Lightning activity as an indicator of climate change , 1999 .

[20]  Tsutomu Takahashi,et al.  Charges on Graupel and Snow Crystals and the Electrical Structure of Winter Thunderstorms , 1999 .

[21]  Robert F. Adler,et al.  Evolution of El Niño‐precipitation relationships from satellites and gauges , 2003 .

[22]  Nicholas Kouwen,et al.  Toward the Use of Coupled Atmospheric and Hydrologic Models at Regional Scale , 2000 .

[23]  Robert F. Adler,et al.  A Proposed Tropical Rainfall Measuring Mission (TRMM) Satellite , 1988 .