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  1. No Access

    Article

    Modelling of 2016 Kumamoto earthquake by integrating site effect in semi-empirical technique

    The 2016 Kumamoto earthquake (MJMA7.3) struck central area of Kyushu Island, Japan. The presence of near surface low velocity layer greatly amplified the ground motions and caused severe damage in this region. Th...

    Sonia Devi, Sandeep, Parveen Kumar, Monika, A. Joshi in Natural Hazards (2022)

  2. No Access

    Article

    Spatial variability studies of attenuation characteristics of Qα and Qβ in Kumaon and Garhwal region of NW Himalaya

    The present work explores the attenuation characteristics of Garhwal and Kumaon regions of northwest Himalaya, India. A comparative study of P- and S-wave quality factors (Qα and Qβ) is used to appreciate the dif...

    Monika, Parveen Kumar, Sandeep, Sushil Kumar, A. Joshi, Sonia Devi in Natural Hazards (2020)

  3. No Access

    Article

    Determination of site effect and anelastic attenuation at Kathmandu, Nepal Himalaya region and its use in estimation of source parameters of 25 April 2015 Nepal earthquake Mw = 7.8 and its aftershocks including the 12 May 2015 Mw = 7.3 event

    The destructive Mw = 7.8 Nepal earthquake happened in Nepal Himalaya, 80 km NW of Kathmandu city on 25 April 2015. A number of aftershocks in which one of them is Mw = 7.3 which occurred on 12 May 2015 are obser...

    Parveen Kumar, A. Joshi, Sushil Kumar, Sandeep, Sohan Lal in Natural Hazards (2018)

  4. No Access

    Article

    Estimation of the source parameters of the Nepal earthquake from strong motion data

    Kathmandu and its surrounding region were rocked recently by a devastating earthquake on April 25, 2015. This is the largest earthquake that has occurred in this region since the past eight decades. This earth...

    A. Joshi, Monu Tomer, Sohan Lal, Sumer Chopra, Sandeep Singh in Natural Hazards (2016)

  5. No Access

    Article

    Simulation of the records of the 27 March 2013 Nantou Taiwan earthquake using modified semi-empirical approach

    It is seen that strong motion generation area plays an important role in the sha** of strong motion records at the observation point. Strong motion generation areas identified within the rupture plane of th...

    A. Joshi, Chun-Hsiang Kuo, Piu Dhibar, Sandeep, M. L. Sharma in Natural Hazards (2015)

  6. No Access

    Article

    Modeling of strong motion generation areas of the Niigata, Japan, earthquake of 2007 using modified semi-empirical technique

    The Niigata prefecture in Japan was devastated by a large shallow earthquake (M w 6.6, M JMA 6.8) on July 16, 2007. This earthquake has been recorded at 305 stations of Kiban Kyos...

    Sandeep, A. Joshi, Kamal, Parveen Kumar, Ashvini Kumar, Piu Dhibar in Natural Hazards (2015)

  7. No Access

    Article

    Coda wave attenuation characteristics for Kumaon and Garhwal Himalaya, India

    Uttarakhand Himalayas are among one of the most seismically active continental regions of the world. The Himalayan belt in this region is divided into Kumaon and Garhwal Himalaya. The Kumaon Himalayas has not...

    Ashvini Kumar, A. Sinvhal, A. Joshi, D. Kumar, Sandeep, Parveen Kumar in Natural Hazards (2015)

  8. No Access

    Article

    Effect of frequency-dependent radiation pattern in the strong motion simulation of the 2011 Tohoku earthquake, Japan, using modified semi-empirical method

    We perform a strong ground motion simulation using a modified semi-empirical technique (Midorikawa in Tectonophysics 218:287–295, 1993), with frequency-dependent radiation pattern model. Joshi et al. (Nat Hazards...

    Sandeep, A. Joshi, Kamal, Parveen Kumar, Ashvini Kumar in Natural Hazards (2014)

  9. No Access

    Article

    Modeling of strong motion generation area of the Uttarkashi earthquake using modified semiempirical approach

    The semiempirical approach based on envelope summation method given by Midorikawa (Tectonophysics 218:287–295, 1993) has been modified in this paper for modeling of strong motion generation areas (SMGAs). Horizon...

    Sandeep, A. Joshi, Kamal, Parveen Kumar, Pushpa Kumari in Natural Hazards (2014)

  10. No Access

    Article

    Modeling of strong motion generation areas of the 2011 Tohoku, Japan earthquake using modified semi-empirical technique

    Modification in the semi-empirical technique for the simulation of strong ground motion has been introduced to incorporate the strong motion generation areas (SMGA) in the modeled rupture plane. Strong motion ...

    A. Joshi, Sandeep, Kamal in Natural Hazards (2014)

  11. Article

    Erratum to: Hybrid attenuation model for estimation of peak ground accelerations in the Kutch region, India

    A. Joshi, Ashvini Kumar, K. Mohan, B. K. Rastogi in Natural Hazards (2014)

  12. No Access

    Article

    Use of site amplification and anelastic attenuation for the determination of source parameters of the Sikkim earthquake of September 18, 2011, using far-field strong-motion data

    An earthquake of magnitude 6.9 (M w) occurred in the Sikkim region of India on September 18, 2011. This earthquake is recorded on strong-motion network in Uttarakhand Himalaya located about 900 km...

    A. Joshi, Parveen Kumar, Sandeep Arora in Natural Hazards (2014)

  13. No Access

    Article

    Simulation of strong ground motion due to great earthquake in the central seismic gap region of Uttarakhand Himalaya

    Uttarakhand Himalaya in India lies in the central seismic gap region identified by Khattri and Tyagi (Tectonophysics 96:281–297, 1983). Most of the area in Uttarakhand state has been placed under zone V (the high...

    Kapil Mohan, A. Joshi in Natural Hazards (2013)

  14. No Access

    Article

    Hybrid attenuation model for estimation of peak ground accelerations in the Kutch region, India

    The Kutch region of Gujarat in India is the locale of one of the most devastating earthquake of magnitude (M w) 7.7, which occurred on January 26, 2001. Though, the region is considered as seismic...

    A. Joshi, Ashvini Kumar, K. Mohan, B. K. Rastogi in Natural Hazards (2013)

  15. No Access

    Article

    Near-field and far-field simulation of accelerograms of Sikkim earthquake of September 18, 2011 using modified semi-empirical approach

    The semi-empirical approach for modeling of strong ground motion given by Midorikawa (Tectonophysics 218:287–295, 1993) has been modified in the present paper for component wise simulation of strong ground motion...

    A. Joshi, Pushpa Kumari, Sandeep Singh, M. L. Sharma in Natural Hazards (2012)

  16. No Access

    Article

    Estimation of model parameter of Sumatra earthquake using empirical Green’s function technique and generation of hypothetical earthquake scenario for Andaman Island, India

    Empirical Green’s function (EGF) technique is considered to be most effective technique for simulation of ground motions due to a finite earthquake source. In the present paper, this technique has been used to...

    A. Joshi, Pushpa Kumari, Sushil Kumar, M. L. Sharma, A. K. Ghosh in Natural Hazards (2012)

  17. No Access

    Article

    Role of attenuation relationship in sha** the seismic hazard

    Attenuation relationships are commonly used for engineering studies to estimate the peak ground acceleration values. This paper presents the role of attenuation relationship in defining the seismic hazard in a...

    K. Mohan, A. Joshi in Natural Hazards (2012)

  18. No Access

    Article

    Expected peak ground acceleration in Uttarakhand Himalaya, India region from a deterministic hazard model

    A method of seismic zonation based on the deterministic modeling of rupture planes is presented. Finite rupture planes along identified lineaments are modeled in the Uttarakhand Himalaya based on the semi empi...

    A. Joshi, K. Mohan in Natural Hazards (2010)

  19. No Access

    Article

    A deterministic approach for preparation of seismic hazard maps in North East India

    A method of seismic zonation based on deterministic modeling of rupture plane is presented in this work. This method is based on the modeling of finite rupture plane along identified lineaments in the region u...

    A. Joshi, Kapil Mohan, R. C. Patel in Natural Hazards (2007)

  20. No Access

    Article

    Inversion of seismic intensity data for the determination of three-dimensional attenuation structures in the central gap region of Himalayas

    The central gap region of Himalaya, which lies in the northern part of the Indian subcontinent, is exposed to great seismic hazard. A three-dimensional attenuation structure (Q) of this region is obtained using t...

    A. Joshi in Natural Hazards (2007)