Time and Tide Wait for No Man

Andrew C. Kemp, Benjamin P. Horton

Research output: Chapter in Book/Report/Conference proceedingChapter

Abstract

Relative sea level is the difference in height between the coast and sea surface. It changes across space and through time in response to many different physical processes operating on a range of scales. Using an example from North Carolina, USA, we introduce some of these key processes and explore how their importance varies on timescales from hours (e.g., hurricanes and tides) to millennia (e.g., ongoing subsidence of the coast). Below the salt marshes of North Carolina (and elsewhere) are sequences of sediment that that accumulated over thousands of years and record relative sea-level changes. Geologists collect this sediment, establish its age and interrogate it to understand when and how relative sea level changed long before people began to make systematic measurements. This research shows that the rate of rise during the twentieth century was without precedent in ~2000 years.

Original languageEnglish (US)
Title of host publicationSpringer Climate
PublisherSpringer Science and Business Media B.V.
Pages33-53
Number of pages21
DOIs
StatePublished - 2021

Publication series

NameSpringer Climate
ISSN (Print)2352-0698
ISSN (Electronic)2352-0701

All Science Journal Classification (ASJC) codes

  • Global and Planetary Change
  • Atmospheric Science
  • Management, Monitoring, Policy and Law

Keywords

  • Fieldwork
  • Foraminifera
  • Isostasy
  • North Carolina
  • Outer Banks
  • Relative sea level
  • Salt marsh

Fingerprint Dive into the research topics of 'Time and Tide Wait for No Man'. Together they form a unique fingerprint.

Cite this