Mark Cresswell Impacts: Sea-level Change 69EG6517 – Impacts & Models of Climate Change

Topics Introduction Measuring sea-level change Some facts Summary

Introduction The term “sea-level change” refers to a change in the mean-sea-level for sentinel ports across the globe MSL is the average of high and low water marks Tidal surges may occur as a result of storm events – making coastal zones vulnerable but not necessarily due to a change in MSL Sea-level change is primarily due to thermal expansion and not “more water”

Measuring Sea-level Change Changes in sea-level are recorded by the Permanent Service for Mean Sea Level (PSMSL) at the Proudman Oceanographic Laboratory (POL) on Merseyside Tide gauge data from around the world are collated at POL and trends in sea level are derived from time series extending back many decades or even centuries

Measuring Sea-level Change

Sea-level is routinely measured from altimetric satellites such as TOPEX- POSEIDON and JASON The significant wave height is determined from the return time of energy emitted from TOPEX As water expands in response to thermal forcing, TOPEX can be used to derive a proxy of SST as well as wave height

Measuring Sea-level Change

Jason-1 is a new altimetric satellite designed to follow on from the TOPEX POSEIDON mission

Measuring Sea-level Change

Some facts Some components of future sea-level rise can be modelled regionally using coupled ocean- atmosphere models The most common method of obtaining scenarios is to apply global mean estimates from simple models Changes in the occurrence of extreme events such as storm surges can lead to major coastal impacts

Some facts

Global mean sea-level has risen by about mm a year over the past 3000 years and by about 1-2mm a year since 1900 with a central value of 1.5mm per year It is believed (IPCC) that sea-level will rise by metre between 1990 and 2100 Higher MSL will increase the frequency of existing extreme levels associated with storm waves and surges.

Some facts Sea-level will tend to increase in association with a warmer climate as a result of: –Thermal expansion of seawater –Melting of small mountain glaciers and ice caps –Melting of the Greenland ice cap –Changes in the mass balance of the Antarctic ice cap

Some facts As seawater warms, its density decreases – thus a given mass of ocean water will occupy a greater volume as the ocean warms – thereby tending to increase the average sea level A globally uniform ocean warming by 3ºC would cause a sea-level rise of about 2.4 m Complete melting of all mountain glaciers and ice caps is estimated to raise sea level by some 50± 10 cm (Harvey 2000 after Warrick et al. 1996)

Some facts Greenland is of particular concern because of its large ice mass – enough to raise sea-level by about 7.4 m if it was to melt A regional warming of about 6ºC would be sufficient to provoke the eventual melting of the entire ice mass (Letréguilly et al. 1991) Some models show that increased temperatures lead to enhanced snowfall over both Greenland and Antarctic ice sheets – however Greenland ice cores show a reverse relationship

Contribution to SL rise (cm) from 1990 to 2100 (Harvey, 2000) Reference  T (ºC) Glaciers & ice caps GreenlandAntarcticaThermal expansion Total Wigley & Raper (1995) De Wolde et al. (1997) Gregory & Oerlemans (1998) Huybrechts & de Wolde (1999) Bryan (1996) ± 5--