Estuarine response to river flow and sea-level rise under future climate change and human development

2015 ◽  
Vol 156 ◽  
pp. 19-30 ◽  
Author(s):  
Zhaoqing Yang ◽  
Taiping Wang ◽  
Nathalie Voisin ◽  
Andrea Copping
Keyword(s):  
Climate Change ◽  
Sea Level Rise ◽  
Human Development ◽  
Sea Level ◽  
River Flow ◽  
Future Climate ◽  
Future Climate Change ◽  
And Sea Level

scholarly journals Suspended sediment projections in Apalachicola Bay in response to altered river flow and sediment loads under climate change and sea level rise

2016 ◽  
Vol 4 (10) ◽  
pp. 428-439 ◽  
Author(s):  
Wenrui Huang ◽  
Scott C. Hagen ◽  
Dingbao Wang ◽  
Paige A. Hovenga ◽  
Fei Teng ◽  
...  
Keyword(s):  
Climate Change ◽  
Sea Level Rise ◽  
Suspended Sediment ◽  
Sea Level ◽  
River Flow ◽  
Apalachicola Bay ◽  
Sediment Loads ◽  
And Sea Level

Developing future sea level services for Small Island Developing States

2020 ◽  
Author(s):  
Svetlana Jevrejeva ◽  
Judith Wolf ◽  
Andy Matthews ◽  
Joanne Williams ◽  
David Byrne ◽  
...  
Keyword(s):  
Climate Change ◽  
Sea Level Rise ◽  
Water Level ◽  
Sea Level ◽  
Future Climate Change ◽  
Small Island ◽  
Caribbean Region ◽  
Caribbean Islands ◽  
The Caribbean ◽  
And Sea Level

<p>The Caribbean islands encompass some of the most vulnerable coastlines in terms of sea level rise, exposure to tropical cyclones, changes in waves and storm surges. Climate in the Caribbean is already changing and sea level rise impacts are already being felt. Considerable local and regional variations in the rate, magnitude, and direction of sea-level change can be expected as a result of thermal expansion, tectonic movements, and changes in ocean circulation. Governments in the Caribbean recognise that climate change and sea level rise are serious threats to the sustainable development and economic growth of the Caribbean islands and urgent actions are required to increase the resilience and make decisions about how to adapt to future climate change (Caribbean Marine Climate Change Report Card 2017; IPCC 2014).</p><p>As part of the UK Commonwealth Marine Economies (CME) Programme and through collaboration with local stakeholders in St Vincent, we have identified particular areas at risk from changing water level and wave conditions. The Caribbean Sea, particularly the Lesser Antilles, suffers from limited observational data due to a lack of coastal monitoring, making numerical models even more important to fill this gap. The current projects brings together improved access to tide gauge observations, as well as global, regional and local water level and wave modelling to provide useful tools for coastal planners.</p><p>We present our initial design of a coastal data hub with sea level information for stakeholder access in St. Vincent and Grenadines, Grenada and St Lucia, with potential development of the hub for the Caribbean region. The work presented here is a contribution to the wide range of ongoing activities under the Commonwealth Marine Economies (CME) Programme in the Caribbean, falling within the work package “Development of a coastal data hub for stakeholder access in the Caribbean region”, under the NOC led projects “Climate Change Impact Assessment: Ocean Modelling and Monitoring for the Caribbean CME states”.</p>

Future climate change driven sea-level rise: secondary consequences from human displacement for island biodiversity

2012 ◽  
Vol 18 (9) ◽  
pp. 2707-2719 ◽  
Author(s):  
Florian T. Wetzel ◽  
W. Daniel Kissling ◽  
Helmut Beissmann ◽  
Dustin J. Penn
Keyword(s):  
Climate Change ◽  
Sea Level Rise ◽  
Sea Level ◽  
Future Climate ◽  
Future Climate Change ◽  
Island Biodiversity ◽  
Human Displacement

scholarly journals TO THE EFFECTIVENESS OF COASTAL AND FLOOD PROTECTION STRUCTURES UNDER TERMS OF CHANGING CLIMATE CONDITIONS

2012 ◽  
Vol 1 (33) ◽  
pp. 60 ◽  
Author(s):  
Peter Froehle
Keyword(s):  
Climate Change ◽  
Sea Level Rise ◽  
Sea Level ◽  
Wind Field ◽  
Future Climate ◽  
Future Climate Change ◽  
Coastal Protection ◽  
Climate Conditions ◽  
Average Wind ◽  
The World

Consequences resulting from future Climate Change may be one of the most severe threats for people and economies in many countries of the world. Besides the problem of sea level rise, also possible general changes in the frequency and intensity of storms as well as general changes in the average wind field are expected for the future. With respect to the coastal protection possible future strategies and also possible future measure are analyzed and assessed with the result that technical, morphological, socio-economic and aesthetical aspects play a role.

A radiocarbon chronology of Holocene climate change and sea-level rise at the Delmarva Peninsula, US Mid-Atlantic Coast

The Holocene ◽  
2021 ◽  
pp. 095968362110482
Author(s):  
Kelvin W Ramsey ◽  
Jaime L. Tomlinson ◽  
C. Robin Mattheus
Keyword(s):  
Climate Change ◽  
North America ◽  
Sea Level Rise ◽  
Sea Level ◽  
Early Holocene ◽  
Eastern North America ◽  
Delmarva Peninsula ◽  
The Holocene ◽  
Cool Climate ◽  
And Sea Level

Radiocarbon dates from 176 sites along the Delmarva Peninsula record the timing of deposition and sea-level rise, and non-marine wetland deposition. The dates provide confirmation of the boundaries of the Holocene subepochs (e.g. “early-middle-late” of Walker et al.) in the mid-Atlantic of eastern North America. These data record initial sea-level rise in the early Holocene, followed by a high rate of rise at the transition to the middle Holocene at 8.2 ka, and a leveling off and decrease in the late-Holocene. The dates, coupled to local and regional climate (pollen) records and fluvial activity, allow regional subdivision of the Holocene into six depositional and climate phases. Phase A (>10 ka) is the end of periglacial activity and transition of cold/cool climate to a warmer early Holocene. Phase B (10.2–8.2 ka) records rise of sea level in the region, a transition to Pinus-dominated forest, and decreased non-marine deposition on the uplands. Phase C (8.2–5.6 ka) shows rapid rates of sea-level rise, expansion of estuaries, and a decrease in non-marine deposition with cool and dry climate. Phase D (5.6–4.2 ka) is a time of high rates of sea-level rise, expanding estuaries, and dry and cool climate; the Atlantic shoreline transgressed rapidly and there was little to no deposition on the uplands. Phase E (4.2–1.1 ka) is a time of lowering sea-level rise rates, Atlantic shorelines nearing their present position, and marine shoal deposition; widespread non-marine deposition resumed with a wetter and warmer climate. Phase F (1.1 ka-present) incorporates the Medieval Climate Anomaly and European settlement on the Delmarva Peninsula. Chronology of depositional phases and coastal changes related to sea-level rise is useful for archeological studies of human occupation in relation to climate change in eastern North America, and provides an important dataset for future regional and global sea-level reconstructions.

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