SELFE case studies - Revision history

Yjzhang: /* Columbia River estuary and plume */

2013-02-01T14:26:24Z

‎Columbia River estuary and plume

2013-01-18T19:57:03Z

2012-10-19T12:12:34Z

2012-10-19T11:05:02Z

‎Marine Submersion (Xynthia Storm Surge)

2012-10-19T11:00:59Z

‎Marine Submersion (Xynthia Strom Surge)

2012-10-18T21:21:07Z

‎Marine Submersion (Xynthia Strom Surge)

2012-10-18T21:19:15Z

‎Marine Submersion (Xynthia Strom Surge)

2012-10-18T19:28:23Z

‎Tsunami

2012-10-18T16:36:12Z

‎Xavier's group

2012-10-18T16:28:39Z

@@ Line 11: / Line 11: @@
 [http://www.stccmop.org/datamart/virtualcolumbiariver '''Project web site''']<br/>
+[http://tidesandcurrents.noaa.gov/ofs/creofs/creofs.html '''SELFE-enabled Columbia River forecast system at NOAA''']<br/>
 '''Related publications'''<br>

← Older revision		Revision as of 19:57, 18 January 2013
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	Fig. 1 shows the Columbia River plume in 3D view forecasted by SELFE.		Fig. 1 shows the Columbia River plume in 3D view forecasted by SELFE.
	[[File:Virtual-CR.png\|thumb\|center\|Fig. 1 3D view of the Columbia River plume]]<br/>		[[File:Virtual-CR.png\|thumb\|center\|Fig. 1 3D view of the Columbia River plume]]<br/>
		+
		+	==SESAME==
		+	[http://sesame.noaa.gov/sesame.html '''Project web site''']<br/>

← Older revision		Revision as of 12:12, 19 October 2012
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	Fig. 1 shows the Columbia River plume in 3D view forecasted by SELFE.		Fig. 1 shows the Columbia River plume in 3D view forecasted by SELFE.
	[[File:Virtual-CR.png\|thumb\|center\|Fig. 1 3D view of the Columbia River plume]]<br/>		[[File:Virtual-CR.png\|thumb\|center\|Fig. 1 3D view of the Columbia River plume]]<br/>
−
−	~~==DWR==~~

@@ Line 60: / Line 60: @@
 <br/>
 '''Projection description'''<br/>
-In February 2010, the storm Xynthia hit the central part of the Bay of Biscay severely. The storm surge locally exceeded 1.5m (Bertin et al., 2011) and peaked at the same time as a high spring tide, causing the flooding of large areas of the low-lying coast. Analysis results show the wave processes are important in the storm surge. The 2DH SELFE with WWM coupled model was applied in the research. And a highly refined flooding grid was developed to catch the pysical processes of flooding.<br/>
+In February 2010, the storm Xynthia hit the central part of the Bay of Biscay severely. The storm surge locally exceeded 1.5m (Bertin et al., 2011) and peaked at the same time as a high spring tide, causing the flooding of large areas of the low-lying coast. Analysis results show the wave processes are important in the storm surge. The 2DH SELFE with WWM coupled model was applied in the research. And a highly refined flooding multiscale grid was developed to catch the pysical processes of flooding.<br/>

@@ Line 55: / Line 55: @@
 <br/>
-==Marine Submersion (Xynthia Strom Surge)==
+==Marine Submersion (Xynthia Storm Surge)==
 '''Research Team'''<br/>
 DPL: Xavier Bertin, Kai Li, Aron Roland, Nicolas Bruneau, Jean-François Breilh et al.<br/>

@@ Line 70: / Line 70: @@
 '''Sample images'''<br/>
-Fig. 3 Simulation Water depth in North of La Rochelle during Xynthia
+Fig. 3 shows the simulated water depth in North of La Rochelle during Xynthia of preliminary result.
-[[File:Xynthia flooding.png|thumb|center|Fig. 3 Simulated Water depth in North of La Rochelle during Xynthia (red line: observed flooding boundary]]<br/>
+[[File:Xynthia flooding.png|thumb|center|Fig. 3 Simulated water depth in North of La Rochelle during Xynthia (red line: observed flooding boundary]]<br/>
 ==Portuguese coastal systems==

@@ Line 143: / Line 143: @@
 Report 436p.
    <LI>Priest, G.R., Goldfinger, C., Wang, K., Witter, R.C., Zhang, Y., Baptista, A.M. (2010) Confidence levels for tsunami-inundation limits in northern Oregon inferred from a 10,000-year history of great earthquakes at the Cascadia subduction zone. Natural Hazards, 54(1), 27-73.
-   <LI>Witter, R.C, Zhang, Y., Wang, K., Goldfinger, C., Priest, G.R., Allan, J.C. (in press) Coseismic slip on the Cascadia megathrust implied by tsunami deposits in an Oregon lake. Journal of Geophysical Research-Solid Earth.
+   <LI>Witter, R.C, Zhang, Y., Wang, K., Goldfinger, C., Priest, G.R., Allan, J.C. (2012) Coseismic slip on the Cascadia megathrust implied by tsunami deposits in an Oregon lake. Journal of Geophysical Research-Solid Earth, 117, B10303, doi:10.1029/2012JB009404.
    <LI>Witter, R.C., Jaffe, B., Zhang, Y. and Priest, G.R. (2011) Reconstructing hydrodynamic flow parameters of the 1700 tsunami at Cannon Beach, Oregon, USA., Natural Hazards, DOI 10.1007/s11069-011-9912-7.
    <LI>Zhang, Y., Witter, R.W. and Priest, G.P. (2011) Tsunami-Tide Interaction in 1964 Prince William Sound Tsunami, Ocean Modelling, 40, 246-259.

@@ Line 70: / Line 70: @@
 '''Sample images'''<br/>
-Fig. 3 Simulated Water depth in North of La Rochelle during Xynthia.
+Fig. 3 Flooding grid of Xynthia with bathymetry
-[[File:Xynthia flooding.png|thumb|center|Fig. 3 Simulated Water depth in North of La Rochelle during Xynthia]]<br/>
+[[File:Flooding grid lr.jpg|thumb|center|Fig. 3 Flooding grid of Xynthia with bathymetry]]<br/>
 ==Portuguese coastal systems==

← Older revision		Revision as of 16:28, 18 October 2012
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	Fig. 7 shows SELFE Matlab GUI (currently under development) with a bathymetric map of the Marlborough Sounds, New Zealand.		Fig. 7 shows SELFE Matlab GUI (currently under development) with a bathymetric map of the Marlborough Sounds, New Zealand.
−	[[File:SELFE_GUI.PNG\|thumb\|center\|Fig. 6 SELFE Matlab GUI showing bathymetric map of the Marlborough Sounds, New Zealand]]<br/>	+	[[File:SELFE_GUI.PNG\|thumb\|center\|Fig. 7 SELFE Matlab GUI showing bathymetric map of the Marlborough Sounds, New Zealand]]<br/>