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Arias intensity

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Journal Article
Published: 31 March 2022
Seismological Research Letters (2022) 93 (3): 1619–1635.
...Jinjun Hu; Chaoyue Jin; Hui Zhang; Lei Hu; Zhongwei Wang Abstract The Kanto region is an earthquake disaster‐prone area where it is necessary to conduct regional seismic hazard analysis. Ground‐motion models (GMMs) of Arias intensity, cumulative absolute velocity, and significant duration...
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Journal Article
Published: 16 November 2021
Bulletin of the Seismological Society of America (2022) 112 (2): 1149–1160.
...Xuejing Li; Weijin Xu; Mengtan Gao ABSTRACT Arias intensity ( I A ), as an important seismic parameter, which contains the information of amplitude, frequencies, and duration of ground motion, plays a crucial role in characterizing seismic hazard such as earthquake‐induced landslides...
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Journal Article
Published: 01 February 2021
Earthquake Spectra (2023) 37 (1): 428–448.
... for the energy content of ground motions, Arias Intensity has proved to be efficient in several applications, including the prediction of earthquake-induced slope failure and damage in structures, and to a lesser extent liquefaction triggering. In this article, the Kiban-Kyoshin network (KiK)-net database...
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Journal Article
Published: 03 March 2020
Bulletin of the Seismological Society of America (2020) 110 (2): 508–518.
...Ali Farhadi; Shahram Pezeshk ABSTRACT In this study, we use the referenced empirical method of Atkinson (2008) to develop a ground‐motion model (GMM) for estimating Arias intensity ( I A ) and cumulative absolute velocity (CAV) for the central and eastern North America. We use Campbell...
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Journal Article
Published: 01 August 2019
Earthquake Spectra (2019) 35 (3): 1289–1310.
...Kenneth W. Campbell, M. EERI; Yousef Bozorgnia, M. EERI We updated our Next Generation Attenuation (NGA)-West1 ground motion models (GMMs) for the horizontal components of Arias intensity (AI) and cumulative absolute velocity (CAV) using the functional form and NGA-West2 database we used to develop...
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Journal Article
Published: 18 June 2019
Bulletin of the Seismological Society of America (2019) 109 (4): 1343–1357.
...Jorge Macedo; Norman Abrahamson; Jonathan D. Bray Abstract Conditional ground‐motion models (CGMMs) for estimating Arias intensity ( I A ) for earthquakes in subduction zones are developed. The estimate of I A is conditioned in these models on the estimated peak ground acceleration (PGA...
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Journal Article
Published: 25 September 2017
Bulletin of the Seismological Society of America (2017) 107 (5): 2293–2309.
...Zach Bullock; Shideh Dashti; Abbie Liel; Keith Porter; Zana Karimi; Brendon Bradley Abstract This article presents the development of ground‐motion prediction equations for the maximum rotated (RotD100) horizontal component of five intensity measures: Arias intensity, cumulative absolute velocity...
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Journal Article
Published: 02 August 2016
Bulletin of the Seismological Society of America (2016) 106 (5): 2168–2176.
...Jia Mei Liu; Tao Wang; Shu Ren Wu; Meng Tan Gao Abstract Arias intensity ( I A ) and peak ground acceleration ( PGA ) have been widely used as measures of the intensity of strong ground motions. This study employs a large set of data consisting of 7034 horizontal and 3474 vertical strong‐motion...
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Journal Article
Published: 12 January 2016
Bulletin of the Seismological Society of America (2016) 106 (1): 174–188.
... into account the characteristics of seismicity affecting Greece, we calculated occurrence probabilities for different levels of seismic shaking expressed in terms of Arias intensity for a time interval of 50 yrs. Then, by utilizing the linkage of Newmark displacement with Arias intensity and critical...
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Journal Article
Published: 21 July 2015
Bulletin of the Seismological Society of America (2015) 105 (4): 1903–1918.
...Roxane Foulser‐Piggott; Katsuichiro Goda Abstract Arias intensity ( I A ) and cumulative absolute velocity ( CAV ) are ground‐motion measures that have been found to be well suited to application in a number of problems in earthquake engineering. Both measures reflect multiple characteristics...
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Journal Article
Published: 19 May 2015
Bulletin of the Seismological Society of America (2015) 105 (3): 1768–1778.
...Jia Mei Liu; Meng Tan Gao; Jun Ju Xie Abstract Arias intensity is a measure of earthquake intensity that captures the potential destructiveness of an earthquake. Using the strong ground motion records of the M w 7.6 Chi‐Chi earthquake, Taiwan, we analyze the spatial distribution of the vertical...
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Journal Article
Published: 01 April 2013
Bulletin of the Seismological Society of America (2013) 103 (2A): 1117–1129.
... ), Arias intensity (Ia), and spectral accelerations (SA) using a total number of more than 1500 earthquake records from nine recent earthquakes occurred in Taiwan, California, and Japan. The results indicate that the spatial correlations for these IM s are closely related to the regional site conditions...
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Journal Article
Published: 01 August 2012
Earthquake Spectra (2012) 28 (3): 931–941.
...Kenneth W. Campbell, M. EERI; Yousef Bozorgnia, M. EERI Arias intensity (AI) and cumulative absolute velocity (CAV) have been proposed as instrumental intensity measures that can incorporate the cumulative effects of ground motion duration and intensity on the response of structural...
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Journal Article
Published: 01 February 2012
Bulletin of the Seismological Society of America (2012) 102 (1): 129–142.
...Chyi‐Tyi Lee; Bow‐Shan Hsieh; Chih‐Hsuan Sung; Po‐Shen Lin Abstract The Arias intensity is a measure of earthquake intensity arrived at through the integration of a square of the acceleration time history. It has been demonstrated to be an effective predictor of earthquake damage potential...
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Image
Eight-floor buildings seismic input: distribution of arias intensity (AI, a) and significant duration (SD5-75, b) average values for the 167,960 suites of 11 records that can be constructed from the combination of the 20 records in each set.
Published: 01 November 2023
Figure 7. Eight-floor buildings seismic input: distribution of arias intensity (AI, a) and significant duration (SD5-75, b) average values for the 167,960 suites of 11 records that can be constructed from the combination of the 20 records in each set.
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Arias intensity comparison for the scaled recorded bi-directional ground motion (No. 1, RSN 209 in Table 3) and the RotD100 spectral-compatible acceleration using the previous version and proposed method.
Published: 01 August 2023
Figure 16. Arias intensity comparison for the scaled recorded bi-directional ground motion (No. 1, RSN 209 in Table 3 ) and the RotD100 spectral-compatible acceleration using the previous version and proposed method.
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Arias intensity residuals as a function of the maximum shear strain for EQL and NL.
Published: 01 May 2023
Figure 5. Arias intensity residuals as a function of the maximum shear strain for EQL and NL. EQL: equivalent-linear; NL: nonlinear.
Image
Arias intensity residuals as a function of VS30 and f0 for the EQL and NL analyses.
Published: 01 May 2023
Figure 10. Arias intensity residuals as a function of V S30 and f 0 for the EQL and NL analyses. EQL: equivalent-linear; NL: nonlinear.
Image
Violin plots showing the distribution of Arias intensity (AI, left) and significant duration(SD5-75, right) average values for the 167,960 suites of 11 records that can be constructed from the combination of the 20 records in each set.
Published: 01 May 2022
Figure 3. Violin plots showing the distribution of Arias intensity (AI, left) and significant duration(SD5-75, right) average values for the 167,960 suites of 11 records that can be constructed from the combination of the 20 records in each set.
Image
Left: ratios of Arias intensity (matched/scaled) for each record in the spectrally matched sets as function of the corresponding amplitude-scaled record AI. Right: same as left but for the significant duration SD5-75. (Dashed lines are shown for clarity, but do not imply a sequence or order to the individual data points).
Published: 01 May 2022
Figure 2. Left: ratios of Arias intensity (matched/scaled) for each record in the spectrally matched sets as function of the corresponding amplitude-scaled record AI. Right: same as left but for the significant duration SD5-75. (Dashed lines are shown for clarity, but do not imply a sequence