Energy Corridor - Residual Elevation and Flood Risk

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BP Westlake Complex Shell Woodcreek Complex ConocoPhill ips Main Campus Energy Center Complex Residual Elevation Surface West Houston I-10 / Energy Corridor – 1:10,000 Zoom (World Street Map, Terrain Residual, Multi-Directional Hillshade) Constructed by D Tolman, [email protected] Relati ve Elevat ion Hig h Low I-10 Buffalo Bayou Turkey Creek Langham Creek

Transcript of Energy Corridor - Residual Elevation and Flood Risk

Page 1: Energy Corridor - Residual Elevation and Flood Risk

BP Westlake Complex

Shell Woodcreek Complex

ConocoPhillips Main Campus

Energy Center

Complex

Residual Elevation SurfaceWest Houston I-10 / Energy Corridor – 1:10,000 Zoom

(World Street Map, Terrain Residual, Multi-Directional Hillshade)Constructed by D Tolman, [email protected]

Relative Elevation

High

Low

I-10

Buffalo Bayou

Turkey Creek

Langham Creek

Page 2: Energy Corridor - Residual Elevation and Flood Risk

BP Westlake Complex

Shell Woodcreek Complex

ConocoPhillips Main Campus

Energy Center

Complex

Residual Elevation Surface & FEMAWest Houston I-10 / Energy Corridor – 1:10,000 Zoom

(World Street Map, Terrain Residual, Multi-Directional Hillshade)Constructed by D Tolman, [email protected]

Relative Elevation

High

Low

I-10

FEMA Floodway

FEMA 500 yr Floodplain

FEMA 100 yr Floodplain

Page 3: Energy Corridor - Residual Elevation and Flood Risk

Discussion:

• The first image is an enlargement of the Energy Corridor showing three layers: World Street Map, Multi-Directional Hillshade and the Residual Map of the LIDAR Elevation Surface. The colors clearly show the relative elevation highs and lows in the Energy Corridor area. The second image shows the FEMA flood designations superimposed on the map. I believe that the two are in close agreement, particularly along the drainage systems.

• There are differences however, likely due to FEMA’s focus on localized flooding along streams and channels. Alternatively, the residual map shows all local low areas, even those not adjacent to streams. I have noted that many of the structures that flooded during the two major flood events of 2016 were not within a FEMA designated flood zone. I suggest that, due to the very low surface gradients in the area, water from extreme rainfall events will temporarily “pool” with local low areas, and cause short-lived flooding outside of FEMA designated areas.

• These extreme rainfall events seem to be more and more common, in which case every foot of elevation matters. Perhaps an increased awareness of this topic would allow the public to make more informed decisions regarding flood insurance.