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2017
DOI: 10.1016/j.jastp.2016.12.018
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Investigation of atmospheric anomalies associated with Kashmir and Awaran Earthquakes

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Cited by 34 publications
(11 citation statements)
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“…Spatial distribution of SLHF peaks compared to the background years during 128-136 Julian days of 2015, red and black stars are the location of main earthquake and aftershock events, respectively. and beyond (ionosphere) (Dunajecka and Pulinets, 2005;Pulinets and Dunajecka, 2007;Daneshvar et al, 2014;Mahmood et al, 2017). Therefore an integrated approach combining land, atmosphere, meteorological and ionospheric parameters is recommended for a relaible information about an impending earthquake (Singh et al, 2010c).…”
Section: Discussionmentioning
confidence: 99%
“…Spatial distribution of SLHF peaks compared to the background years during 128-136 Julian days of 2015, red and black stars are the location of main earthquake and aftershock events, respectively. and beyond (ionosphere) (Dunajecka and Pulinets, 2005;Pulinets and Dunajecka, 2007;Daneshvar et al, 2014;Mahmood et al, 2017). Therefore an integrated approach combining land, atmosphere, meteorological and ionospheric parameters is recommended for a relaible information about an impending earthquake (Singh et al, 2010c).…”
Section: Discussionmentioning
confidence: 99%
“…The general anomaly method is to find the difference between current data during an earthquake and the long-term average value (also called a reference value) in order to improve result robustness and eliminate potential bias (Mahmood et al, 2017;Qin et al, 2014a;Wu et al, 2016). This method can be expressed as…”
Section: Image Difference Methodsmentioning
confidence: 99%
“…The preliminary step is to identify which precursors present anomalous variations prior to strong earthquakes around the epicenter. OLR, air temperature, and relative humidity were used in the seismic anomaly analysis for the 2005 M w 7.6 Kashmir and 2013 M w 7.7 Awaran earthquakes (Mahmood et al, 2017). Singh et al (2007) analyzed changes in SLHF, atmospheric water vapor, SST, wind, cloud liquid water, precipitation rate, and chlorophyll concentrations prior to and after the 2004 Sumatra earthquake.…”
Section: Multiparameter Comprehensive Analysismentioning
confidence: 99%
“…The general anomaly method is to find the difference between current data during an earthquake and the long-term average value (also called a reference value) in order to improve result robustness and eliminate potential bias (Mahmood et al, 2017;Qin et al, 2014a;Wu et al, 2016). This method can be expressed as…”
Section: Image Difference Methodsmentioning
confidence: 99%