Disruptive Role of Vertical Land Motion in Future Assessments of Climate Change-Driven Sea-Level Rise and Coastal Flooding Hazards in the Chesapeake Bay
| dc.contributor.author | Sherpa, Sonam Futi | en |
| dc.contributor.author | Shirzaei, Manoochehr | en |
| dc.contributor.author | Ojha, Chandrakanta | en |
| dc.coverage.country | United States | en |
| dc.coverage.state | Virginia | en |
| dc.coverage.state | Maryland | en |
| dc.date.accessioned | 2023-04-27T16:49:33Z | en |
| dc.date.available | 2023-04-27T16:49:33Z | en |
| dc.date.issued | 2023-04 | en |
| dc.description.abstract | Future projections of sea-level rise (SLR) used to assess coastal flooding hazards and exposure throughout the 21st century and devise risk mitigation efforts often lack an accurate estimate of coastal vertical land motion (VLM) rate, driven by anthropogenic or non-climate factors in addition to climatic factors. The Chesapeake Bay (CB) region of the United States is experiencing one of the fastest rates of relative sea-level rise on the Atlantic coast of the United States. This study uses a combination of space-borne Interferometric Synthetic Aperture Radar (InSAR), Global Navigation Satellite System (GNSS), Light Detecting and Ranging (LiDAR) data sets, available National Oceanic and Atmospheric Administration (NOAA) long-term tide gauge data, and SLR projections from the Intergovernmental Panel on Climate Change (IPCC), AR6 WG1 to quantify the regional rate of relative SLR and future flooding hazards for the years 2030, 2050, and 2100. By the year 2100, the total inundated areas from SLR and subsidence are projected to be 454(316–549)–600(535𝐴𝐴–690) km² for Shared Socioeconomic Pathways (SSPs) 1–1.9 to 5–8.5, respectively, and 342(132–552)–627(526–735) 𝐴𝐴 km2 only from SLR. The effect of storm surges based on Hurricane Isabel can increase the inundated area to 849(832–867)–1,117(1,054–1,205) km² under different VLM and SLR scenarios. We suggest that accurate estimates of VLM rate, such as those obtained here, are essential to revise IPCC projections and obtain accurate maps of coastal flooding and inundation hazards. The results provided here inform policymakers when assessing hazards associated with global climate changes and local factors in CB, required for developing risk management and disaster resilience plans. | en |
| dc.description.sponsorship | The work of Sonam Futi Sherpa was supported by the US Geological Survey and NASA Grant 80NSSC170567 and in part by the National Science Foundation under Grant 1735139. Any opinions, findings, and conclusions, or recommendations expressed in this material are those of the authors and do not necessarily reflect the views of the National Science Foundation. Manoochehr Shirzaei was supported by the US Geological Survey and partially by NASA Grant 80NSSC170567. The support of the Geological Society of America (GSA) is acknowledged here. We thank the projection authors for developing and making the SLR projections available, multiple funding agencies for supporting the development of the projections, and the NASA Sea-Level Change Team for developing and hosting the IPCC AR6 Sea-Level Projection Tool. | en |
| dc.description.version | Published version | en |
| dc.format.mimetype | application/pdf | en |
| dc.identifier.doi | https://doi.org/10.1002/essoar.10511192.1 | en |
| dc.identifier.uri | http://hdl.handle.net/10919/114830 | en |
| dc.language.iso | en | en |
| dc.publisher | American Geophysical Union | en |
| dc.rights | Creative Commons Attribution 4.0 International | en |
| dc.rights.uri | http://creativecommons.org/licenses/by/4.0/ | en |
| dc.title | Disruptive Role of Vertical Land Motion in Future Assessments of Climate Change-Driven Sea-Level Rise and Coastal Flooding Hazards in the Chesapeake Bay | en |
| dc.title.serial | Journal of Geophysical Research: Solid Earth | en |
| dc.type | Article - Refereed | en |
| dc.type.dcmitype | Text | en |