Rates and causes of recent global sea-level rise inferred from long tide gauge data records [An article from: Quaternary Science Reviews]
Book Details
Author(s)M. Nakada, H. Inoue
PublisherElsevier
ISBN / ASINB000RR3XQO
ISBN-13978B000RR3XQ3
MarketplaceFrance 🇫🇷
Description
This digital document is a journal article from Quaternary Science Reviews, published by Elsevier in 2005. The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.
Description:
Tide gauge data at seven sites of the Permanent Service for Mean Sea Level (PSMSL), with information for relative sea-level during the past 140-200yr, were analyzed to examine the rates and causes of the global sea-level rise (GSLR) during the twentieth century. By subtracting linear trends for relative sea-level rise during the past 100yr from the observed data, we get the apparent GSLRs of ~1mmyr^-^1 for five sites around the Baltic Sea and Brest. The rate for San Francisco is significantly larger than this, with an optimum value ~2mmyr^-^1. The spatial difference of ~1mmyr^-^1 between these sites is reasonably explained by the recent melting of the Greenland ice sheet with an equivalent sea-level rise of ~1mmyr^-^1. The predicted relative sea-level change for this melting scenario is 0.5mmyr^-^1 at sites around the Baltic Sea and Brest, and 1.5mmyr^-^1 for San Francisco. The residuals between observations and predictions, ~0.5mmyr^-^1 at all sites, may be contributed by thermal expansion of seawater and/or other melting sources. These results suggest the rate of twentieth-century GSLR to be 1.5mmyr^-^1.
Description:
Tide gauge data at seven sites of the Permanent Service for Mean Sea Level (PSMSL), with information for relative sea-level during the past 140-200yr, were analyzed to examine the rates and causes of the global sea-level rise (GSLR) during the twentieth century. By subtracting linear trends for relative sea-level rise during the past 100yr from the observed data, we get the apparent GSLRs of ~1mmyr^-^1 for five sites around the Baltic Sea and Brest. The rate for San Francisco is significantly larger than this, with an optimum value ~2mmyr^-^1. The spatial difference of ~1mmyr^-^1 between these sites is reasonably explained by the recent melting of the Greenland ice sheet with an equivalent sea-level rise of ~1mmyr^-^1. The predicted relative sea-level change for this melting scenario is 0.5mmyr^-^1 at sites around the Baltic Sea and Brest, and 1.5mmyr^-^1 for San Francisco. The residuals between observations and predictions, ~0.5mmyr^-^1 at all sites, may be contributed by thermal expansion of seawater and/or other melting sources. These results suggest the rate of twentieth-century GSLR to be 1.5mmyr^-^1.
