Response of streamflow to multiple earthquakes
We analyze the streamflow response of Sespe Creek, CA, to several large earthquakes. We find that flow increased after three earthquakes, and that the observed changes in flow have the same character. Both those earthquakes that induced static extension and those that induced static contraction caus...
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| Veröffentlicht in: | Geophysical research letters 2003-03, Vol.30 (5), p.18.1-n/a |
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| container_title | Geophysical research letters |
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| creator | Manga, Michael Brodsky, Emily E. Boone, Michael |
| description | We analyze the streamflow response of Sespe Creek, CA, to several large earthquakes. We find that flow increased after three earthquakes, and that the observed changes in flow have the same character. Both those earthquakes that induced static extension and those that induced static contraction cause flow to increase; streamflow thus appears to respond to dynamic strain. We find that all postseismic responses can be explained by a model in which pore pressure increases coseismically without any changes in hydraulic diffusivity. There is a particle velocity threshold in the range of 5–20 cm/s to induce the pore pressure increase. |
| doi_str_mv | 10.1029/2002GL016618 |
| format | Article |
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We find that flow increased after three earthquakes, and that the observed changes in flow have the same character. Both those earthquakes that induced static extension and those that induced static contraction cause flow to increase; streamflow thus appears to respond to dynamic strain. We find that all postseismic responses can be explained by a model in which pore pressure increases coseismically without any changes in hydraulic diffusivity. There is a particle velocity threshold in the range of 5–20 cm/s to induce the pore pressure increase.</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1029/2002GL016618</identifier><identifier>CODEN: GPRLAJ</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>consolidation ; Earth sciences ; Earth, ocean, space ; earthquakes ; Earthquakes, seismology ; Engineering and environment geology. 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Res. Lett</addtitle><description>We analyze the streamflow response of Sespe Creek, CA, to several large earthquakes. We find that flow increased after three earthquakes, and that the observed changes in flow have the same character. Both those earthquakes that induced static extension and those that induced static contraction cause flow to increase; streamflow thus appears to respond to dynamic strain. We find that all postseismic responses can be explained by a model in which pore pressure increases coseismically without any changes in hydraulic diffusivity. There is a particle velocity threshold in the range of 5–20 cm/s to induce the pore pressure increase.</description><subject>consolidation</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>earthquakes</subject><subject>Earthquakes, seismology</subject><subject>Engineering and environment geology. Geothermics</subject><subject>Exact sciences and technology</subject><subject>Freshwater</subject><subject>Hydrology</subject><subject>Hydrology. 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Geothermics</topic><topic>Exact sciences and technology</topic><topic>Freshwater</topic><topic>Hydrology</topic><topic>Hydrology. 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Res. Lett</addtitle><date>2003-03</date><risdate>2003</risdate><volume>30</volume><issue>5</issue><spage>18.1</spage><epage>n/a</epage><pages>18.1-n/a</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>We analyze the streamflow response of Sespe Creek, CA, to several large earthquakes. We find that flow increased after three earthquakes, and that the observed changes in flow have the same character. Both those earthquakes that induced static extension and those that induced static contraction cause flow to increase; streamflow thus appears to respond to dynamic strain. We find that all postseismic responses can be explained by a model in which pore pressure increases coseismically without any changes in hydraulic diffusivity. 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| ispartof | Geophysical research letters, 2003-03, Vol.30 (5), p.18.1-n/a |
| issn | 0094-8276 1944-8007 |
| language | eng |
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| source | Wiley Online Library Journals Frontfile Complete; Wiley Online Library Free Content; Wiley-Blackwell AGU Digital Library; EZB-FREE-00999 freely available EZB journals |
| subjects | consolidation Earth sciences Earth, ocean, space earthquakes Earthquakes, seismology Engineering and environment geology. Geothermics Exact sciences and technology Freshwater Hydrology Hydrology. Hydrogeology Internal geophysics liquefaction Natural hazards: prediction, damages, etc pore pressure streamflow |
| title | Response of streamflow to multiple earthquakes |
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