Spatial Relation between Wind Stress and Storm Surge during Hurricanes Laura and Delta in 2020
Coastal Studies Institute , Louisiana State University, Baton Rouge, LA 70803, USA
Academic Editor: Zed Rengel
Received: July 25, 2021 | Accepted: August 31, 2021 | Published: September 02, 2021
Adv Environ Eng Res 2021, Volume 2, Issue 3, doi: 10.21926/aeer.2103022
Recommended citation: Hsu SA. Spatial Relation between Wind Stress and Storm Surge during Hurricanes Laura and Delta in 2020. Adv Environ Eng Res 2021; 2(3): 022; doi: 10.21926/aeer.2103022.
© 2021 by the authors. This is an open access article distributed under the conditions of the Creative Commons by Attribution License, which permits unrestricted use, distribution, and reproduction in any medium or format, provided the original work is correctly cited.
In 2020 Hurricanes Laura and Delta devastated southwest and south central coasts of Louisiana (LA), see Tropical Cyclone (TC) Reports by the National Hurricane Center (www.nhc.noaa.gov) [1,2], respectively. Based on these reports, storm surge is defined as the water height above normal astronomical tide level and estimated inundation is the maximum height of water above ground. According to the National Weather Service (NWS) Office in Lake Charles, LA, as shown in Figure 1 and Figure 2, the inundation was up to 18 ft (5.5 m) for Laura and to 10 ft (3 m) for Delta, respectively. During a TC, the Regional and Mesoscale Meteorology Branch (RAMMB) of NOAA/NESDIS issues a Multi-Platform TC Surface Wind Analysis once in every 3 hours worldwide. The isotach (equal wind speed line) maps near landfall during Laura and Delta are presented in Figure 3 and Figure 4, respectively.
Figure 1 Estimated inundation height in southwest LA impacted by Hurricane Laura in 2020 based on https://www.weather.gov/images/lch/events/2020Laura/SW%26SC-Louisiana.png.
Figure 2 Estimated inundation height in south central LA impacted by Hurricane Delta in 2020 based on https://www.weather.gov/images/lch/events/2020Delta/SW%26SC-Louisiana.png.
Figure 3 An isotach map near Laura’s landfall at southwest coast of LA at 06UTC on 27 August 2020 based on https://rammb-data.cira.colostate.edu/tc_realtime/image_mpsatwnd.asp?product=mpsatwnd&storm_identifier=al132020&product_filename=2020al13_mpsatwnd_202008270600.
Figure 4 An isotach map near Delta’s landfall at south central coast of LA at 00UTC on 10 October 2020 based on https://rammb-data.cira.colostate.edu/tc_realtime/image_mpsatwnd.asp?product=mpsatwnd&storm_identifier=al262020&product_filename=2020al26_mpsatwnd_202010100000.
According to Hsu [3,4], most storm surges can be explained by the effect of wind stress using S = 0.005V2, here S is the storm surge in meters and V is the wind speed in m s -1. From Figure 3, the area inside of 65 knots (34 m s -1) isotach should have experienced up to 5.6 m or 18 ft storm surge. This is in reasonable agreement spatially with the area inside of 14 ft inundation line if we add a few feet of topography. Similarly, from Figure 4, the area inside od 50 knots (26 m s -1) isotach should have the storm surge up to 3.3 m or approximately 11 ft. Again, this is in fair agreement with the area inside of 10 ft inundation line. Therefore, it is concluded that the isotach map near a TC’s landfall may be useful for coastal environmental and structural engineering applications. Note that improvements may be made that if the GIS (geographic information system) used by NWS and RAMMB can be unified.
During the review process, three questions were raised: the first one is related to the validity of the wind-stress tide equation, i.e., S = 0.005 V2. A verification of this formula is presented in Table 1 based on the information provided by Figure 4 and Figure 5 and Cangialosi et al. (2020, page 17). Because the National Ocean Service (NOS) station at FRWL1 was damaged by Laura, 3 NOS stations during Delta are employed. Note that, according to Cangialosi et al. 2020, since the storm surge as listed in the last column of Table 1 is the measured water height above normal astronomical tide level which is consistent with that of computed wind-stress tide value, our proposed method is reasonable. The second question is related to the wind direction and storm surge, the answer is provided in Figure 4 and Figure 5 that all three stations as listed in Table 1 had onshore wind direction, indicating that the storm surges were induced by the direct onshore flow. The last question is related to the effect of astronomical tide on the storm surge. The answer is provided in Cangialosi et al. (2020, page 17) that the difference between storm surge and storm tide in our study area is (9.45 – 9.39) = 0.06ft for FRWL1 and (6.40 – 6.44) = -0.04ft for AMRL1, indicating the effects of astronomical are small during Delta. Note that the storm tide is water height above the North American Vertical Datum of 1988 (NAVD88).
Figure 5 Location map from the National Data Buoy Center (NDBC) for the National Ocean Service (NOS) stations at FRWL1, AMRL1 and GISL1 used in Table 1. See https://www.ndbc.noaa.gov/images/maps/WestGulf_inset.gif.
Maps, charts and datasets provided by the NWS Office in Lake Charles, LA, the RAMMB, NHC, NDBC, and NOS used in this brief report are greatly appreciated.
The author did all the research work of this study.
The authors have declared that no competing interests exist.
- Pasch RJ, Berg R, Roberts DP, Papin PP. Tropical cyclone report, Hurricane Laura, 2020. Miami-Dade County, FL: National Hurricane Center; 2020; AL132020.
- Cangialosi JP, Berg R. Tropical cyclone report, Hurricane Delta, 2020. Miami-Dade County, FL: National Hurricane Center; 2021; AL262020.
- Hsu SA. Storm surges in New York during Hurricane Sandy in 2012: A verification of the wind-stress tide relation. Boundary Layer Meteorol. 2013; 148: 593-598. [CrossRef]
- Hsu SA. Storm surge measurements in Naples, Florida, during Hurricane Irma in 2017. Mar Weather Log. 2017; 61: 61-62.