The 2010 Pakistan Flood and Russian Heat Wave: Teleconnection of Hydrometeorological Extremes

AbstractIn this paper, preliminary results are presented showing that the two record-setting extreme events during 2010 summer (i.e., the Russian heat wave–wildfires and Pakistan flood) were physically connected. It is found that the Russian heat wave was associated with the development of an extraordinarily strong and prolonged extratropical atmospheric blocking event in association with the excitation of a large-scale atmospheric Rossby wave train spanning western Russia, Kazakhstan, and the northwestern China–Tibetan Plateau region. The southward penetration of upper-level vorticity perturbations in the leading trough of the Rossby wave was instrumental in triggering anomalously heavy rain events over northern Pakistan and vicinity in mid- to late July. Also shown are evidences that the Russian heat wave was amplified by a positive feedback through changes in surface energy fluxes between the atmospheric blocking pattern and an underlying extensive land region with below-normal soil moisture. The Pakis...

[1]  Pedro Viterbo,et al.  The European Summer of 2003: Sensitivity to Soil Water Initial Conditions , 2006 .

[2]  H. Hsu,et al.  Roles of European blocking and tropical‐extratropical interaction in the 2010 Pakistan flooding , 2011 .

[3]  B. Goswami,et al.  Role of barotropic, baroclinic and combined barotropic-baroclinic instability for the growth of monsoon depressions and mid-tropospheric cyclones , 1980, Journal of Earth System Science.

[4]  Robert A. Houze,et al.  Anomalous Atmospheric Events Leading to the Summer 2010 Floods in Pakistan , 2011 .

[5]  P. Xie,et al.  A Gauge-Based Analysis of Daily Precipitation over East Asia , 2007 .

[6]  S. Schubert,et al.  Warm Season Subseasonal Variability and Climate Extremes in the Northern Hemisphere: The Role of Stationary Rossby Waves , 2011 .

[7]  Y. Hong,et al.  The TRMM Multisatellite Precipitation Analysis (TMPA): Quasi-Global, Multiyear, Combined-Sensor Precipitation Estimates at Fine Scales , 2007 .

[8]  Tao Zhang,et al.  Was there a basis for anticipating the 2010 Russian heat wave? , 2011 .

[9]  Peter J. Webster,et al.  Were the 2010 Pakistan floods predictable? , 2011 .

[10]  M. Mudelsee,et al.  Heterogeneous response of circumboreal wildfire risk to climate change since the early 1900s , 2009 .

[11]  S. Schubert,et al.  MERRA: NASA’s Modern-Era Retrospective Analysis for Research and Applications , 2011 .

[12]  T. Krishnamurti,et al.  Mid-Tropospheric Cyclones of the Southwest Monsoon , 1970 .

[13]  P. Whitfield,et al.  Potential forest fire danger over Northern Eurasia: Changes during the 20th century , 2005 .

[14]  M. Mak The Monsoonal Mid-Tropospheric Cyclogenesis , 1975 .

[15]  R. Gillies,et al.  Pakistan's two-stage monsoon and links with the recent climate change , 2011 .

[16]  Brian J. Hoskins,et al.  Rossby Wave Propagation on a Realistic Longitudinally Varying Flow , 1993 .

[17]  Mid-tropospheric cyclones of the summer monsoon , 1977 .

[18]  Franco Molteni,et al.  On the operational predictability of blocking , 1990 .

[19]  M. Matsueda Predictability of Euro‐Russian blocking in summer of 2010 , 2011 .