Sea level rise in the north-western part of the Arabian Gulf

被引:30
|
作者
Alothman, A. O. [1 ]
Bos, M. S. [2 ]
Fernandes, R. M. S. [2 ]
Ayhan, M. E. [3 ]
机构
[1] King Abdulaziz City Sci & Technol, Space & Aviat Res Inst, Riyadh 11419, Saudi Arabia
[2] Univ Beira Interior, Inst D Luis R Marques dAvila & Boloma, P-6201001 Covilha, Portugal
[3] Middle E Tech Univ, Earthquake Studies Dept, TR-06531 Ankara, Turkey
关键词
Sea level change; Arabian Gulf; GNSS; VULNERABILITY ASSESSMENT; LAND MOTION; KINGDOM; SURFACE; COAST; EARTH; MODEL; GPS;
D O I
10.1016/j.jog.2014.09.002
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Relative sea level variations in the north-western part of the Arabian Gulf have been estimated in the past using no more than 10 to 15 years of observations. In this study, we have almost doubled the period to 28.7 years by examining all available tide gauge data in the area and constructing a mean gauge time-series from seven coastal tide gauges. We found for the period 1979-2007 a relative sea level rise of 2.2 +/- 0.5 mm/year. Using the subsidence observed at 6 GPS stations within a radius of 100 km of the tide gauges as an indication of the vertical land motion, the corresponding absolute sea level rise is 1.5 +/- 0.8 mm/year that is in agreement with the global estimate of 1.9 +/- 0.1 mm/year (Church and White, 2011) for the same studied period. By taking into account the temporal correlations we conclude that previous published results underestimate the true sea level rate uncertainty in this area by a factor of 5-10. (C) 2014 Elsevier Ltd. All rights reserved.
引用
收藏
页码:105 / 110
页数:6
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