Climate Change and Sea-Level Rise

2021 ◽  
Vol 23 (2-3) ◽  
pp. 133-157
Author(s):  
Vladyslav Lanovoy ◽  
Sally O’Donnell

Abstract This article examines the challenges that climate change and sea-level rise pose to certain key aspects of the law of the sea. Sea-level rise is likely to impact maritime baselines, the qualification of maritime features and the entitlements they generate, and ultimately the stability of maritime boundaries, which are critical for the peaceful co-existence of sovereign States. This article examines whether some of the relevant provisions of the United Nations Convention on the Law of the Sea can accommodate a liberal interpretation so as to provide some, even if incomplete, answers to the challenges posed by sea-level rise to the law of the sea regime. It is argued that the legal fiction of permanency that underpins key elements of this legal regime, and thus ignores future physical changes to coastlines, is the most appropriate temporary solution, unless and until new rules are agreed by States to deal comprehensively with sea-level rise.

2018 ◽  
Vol 33 (4) ◽  
pp. 836-846
Author(s):  
Millicent McCreath

Abstract This article summarises and discusses the main issues addressed at the conference hosted by the Centre for International Law at the National University of Singapore in March 2018 on Climate Change and the Law of the Sea: Adapting the Law of the Sea to Address the Challenges of Climate Change. The conference covered topics including the status and entitlement of offshore features, impacts of sea-level rise on baselines, the content of the LOSC climate change obligations, climate change dispute settlement under the LOSC, and possible ways to develop or adapt the LOSC to address the challenges of climate change.


The Holocene ◽  
2021 ◽  
pp. 095968362110482
Author(s):  
Kelvin W Ramsey ◽  
Jaime L. Tomlinson ◽  
C. Robin Mattheus

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.


Sign in / Sign up

Export Citation Format

Share Document