scholarly journals Assessment of Climate Change Impacts on Sea Surface Temperatures and Sea Level Rise—The Arabian Gulf

Climate ◽  
2020 ◽  
Vol 8 (4) ◽  
pp. 50 ◽  
Author(s):  
Mohamed E. Hereher
Keyword(s):  
Coral Reef ◽  
Sea Level Rise ◽  
Sea Level ◽  
Arabian Gulf ◽  
Climate Change Impacts ◽  
Sea Surface ◽  
Coastal Protection ◽  
Positive Trend ◽  
Sea Surface Temperatures ◽  
Surface Temperatures

The Arabian Gulf is one of the regions in the world experiencing major changes due to increased economic growth rates and development practices. As a shallow water body within a hot desert, the Gulf is exposed to obvious warming in the sea surface temperatures (SST). Remotely sensed SST data were utilized to estimate decadal change in SST with a focus on coral reef locations. There is a positive trend in monthly time series SSTs, with a maximum value of about 0.7 °C/decade for the western side of the Gulf. This high trend of SST is associated with significant coral reef bleaching and it coincides with major climate/ocean interactions. Most of the Arabian countries along the Gulf have coastal developments at low-land areas of high vulnerability to sea level rise. Digital elevation models showed that there are more than 3100 km2 of coastal areas that occur at 1 m level along the Arabian countries of the Gulf. Coastal protection and conservation measures are crucial to protect low-lying coasts of urban use.

Remote sensing of the Indo-Pacific region: ocean colour, sea level, winds and sea surface temperatures

2004 ◽  
Vol 25 (7-8) ◽  
pp. 1423-1435 ◽  
Author(s):  
Raghu Murtugudde ◽  
Liping Wang ◽  
Eric Hackert ◽  
James Beauchamp ◽  
James Christian ◽  
...  
Keyword(s):  
Remote Sensing ◽  
Sea Level ◽  
Sea Surface ◽  
Pacific Region ◽  
Sea Surface Temperatures ◽  
Ocean Colour ◽  
Surface Temperatures

Revised Southern Ocean sea surface temperatures over the last 180 ka

2021 ◽  
Author(s):  
David Chandler ◽  
Petra Langebroek
Keyword(s):  
Southern Ocean ◽  
Sea Level ◽  
Climate Model ◽  
Ice Sheet ◽  
Sea Surface ◽  
Sea Surface Temperatures ◽  
Last Interglacial ◽  
Antarctic Ice Sheet ◽  
Surface Temperatures ◽  
Temperature Reconstructions

<p>Proxy records and climate models suggest that the Last Interglacial (LIG, ~130 to 115 thousand years before present) was characterised by high-latitude air and sea surface temperatures (SSTs) slightly warmer than present, and by mean global sea level a few metres higher. Therefore, the LIG is widely used as an analogue for near-future oceanographic/climatic conditions. Of particular interest is the Antarctic Ice Sheet’s contribution to rapid sea level rise and to Southern Ocean surface freshening, in response to warming. In the Southern Ocean, existing LIG temperature reconstructions suffer from very high variance amongst a low number of individual records. Recent syntheses have focused on the LIG climatic optimum, but conditions during the penultimate glacial are also important for forcing transient climate or Antarctic Ice Sheet simulations. Here we use databases of modern core-top sediments to evaluate the strengths of SST proxies available in the Southern Ocean, and consider their likely sources of bias and variance. By selecting only those paleo-temperature reconstructions which we believe are reliable in this region, we then compile a Southern Ocean SST synthesis covering the penultimate glacial and the LIG. This longer temperature time series can be used as a basis for LIG ice sheet simulations or for climate model development.  </p>

scholarly journals Using Historical Responses to Shoreline Change on Australia’s Gold Coast to Estimate Costs of Coastal Adaptation to Sea Level Rise

2020 ◽  
Vol 8 (6) ◽  
pp. 380 ◽  
Author(s):  
Daniel Ware ◽  
Andrew Buckwell ◽  
Rodger Tomlinson ◽  
Kerrie Foxwell-Norton ◽  
Neil Lazarow
Keyword(s):  
Climate Change ◽  
Sea Level Rise ◽  
Sea Level ◽  
Discount Rate ◽  
Coastal Erosion ◽  
Climate Change Impacts ◽  
Coastal Protection ◽  
Social Discount Rate ◽  
Protection Strategy ◽  
Selection Of

Climate change impacts, sea level rise, and changes to the frequency and intensity of storms, in particular, are projected to increase the coastal land and assets exposed to coastal erosion. The selection of appropriate adaptation strategies requires an understanding of the costs and how such costs will vary by the magnitude and timing of climate change impacts. By drawing comparisons between past events and climate change projections, it is possible to use experience of the way societies have responded to changes to coastal erosion to inform the costs and selection of adaptation strategies at the coastal settlement scale. The experience of implementing a coastal protection strategy for the Gold Coast’s southern beaches between 1964 and 1999 is compiled into a database of the timing, units, and cost of coastal protection works. Records of the change to shoreline position and characteristics of local beaches are analysed through the Bruun model to determine the implied sea level rise at the time each of the projects was completed. Finally, an economic model updates the project costs for the point in the future based on the projected timing of sea level rise and calculates a net present value (NPV) for implementing a protection strategy, per km, of sandy beach shoreline against each of the four representative concentration pathways (RCP) of the Intergovernmental Panel on Climate Change (IPCC) to 2100. A key finding of our study is the significant step-up in expected costs of implementing coastal protection between RCP 2.6 and RCP 8.5—from $573,792/km to $1.7 million/km, or a factor of nearly 3, using a social discount rate of 3%. This step-up is by a factor of more than 6 at a social discount rate of 1%. This step-up in projected costs should be of particular interest to agencies responsible for funding and building coastal defences.

scholarly journals The timescale and extent of thermal expansion of the global ocean due to climate change

Ocean Science ◽  
2010 ◽  
Vol 6 (1) ◽  
pp. 179-184 ◽  
Author(s):  
S. Marčelja
Keyword(s):  
Surface Temperature ◽  
Sea Surface Temperature ◽  
Temperature Variation ◽  
Sea Level ◽  
Heat Content ◽  
Sea Surface ◽  
Sea Surface Temperatures ◽  
The Past ◽  
Surface Temperatures

Abstract. With recently improved instrumental accuracy, the change in the heat content of the oceans and the corresponding contribution to the change of the sea level can be determined from in situ measurements of temperature variation with depth. Nevertheless, it would be favourable if the same changes could be evaluated from just the sea surface temperatures because the past record could then be reconstructed and future scenarios explored. Using a single column model we show that the average change in the heat content of the oceans and the corresponding contribution to a global change in the sea level can be evaluated from the past sea surface temperatures. The calculation is based on the time-dependent diffusion equation with the known fixed average upwelling velocity and eddy diffusivity, as determined from the steady-state limit. In this limit, the model reduces to the 1966 Munk profile of the potential temperature variation as a function of depth. There are no adjustable parameters in the calculation and the results are in good agreement with the estimates obtained from the in situ data. The method allows us to obtain relevant timescales and average temperature profiles. The evaluation of the thermosteric sea level change is extended back to the beginning of accurate sea surface temperature records. The changes in sea surface temperature from 1880 until the present time are estimated to have produced a thermosteric sea level rise of 35 mm. Application to future IPCC scenarios gives results similar to the average prediction of more complex climate models.

scholarly journals The timescale and extent of thermal expansion of the oceans due to climate change

2009 ◽  
Vol 6 (3) ◽  
pp. 2975-2992
Author(s):  
S. Marčelja
Keyword(s):  
Surface Temperature ◽  
Sea Surface Temperature ◽  
Temperature Variation ◽  
Sea Level ◽  
Heat Content ◽  
Sea Surface ◽  
Sea Surface Temperatures ◽  
The Past ◽  
Surface Temperatures

Abstract. With recently improved instrumental accuracy, the change in the heat content of the oceans and the corresponding contribution to the change of the sea level can be determined from in situ measurements of temperature variation with depth. Nevertheless, it would be favourable if the same changes could be evaluated from just the sea surface temperatures because the record could then be extended into the past and projected into the future. We show here that the average change in the heat content of the oceans and the corresponding contribution to a change in the sea level can be evaluated from the past sea surface temperatures. The calculation is based on the time-dependent diffusion equation with constant upwelling velocity and has no adjustable parameters. In the steady-state limit it recovers the well-known profile of the potential temperature variation as a function of depth. The results are in good agreement with the estimates obtained from the in situ data, even though most of the warming occurs in the upper 1000 m. The method allows us to obtain relevant timescales and average temperature profiles. The evaluation of the thermosteric sea level change is extended back to the beginning of accurate sea surface temperature records in 1880. The changes in sea surface temperature from 1880 until the present time led to a thermosteric sea level rise of 3 cm and to a commitment for a future rise of 5 cm.

Sea surface temperatures and coral reef bleaching off La Parguera, Puerto Rico (northeastern Caribbean Sea)

Coral Reefs ◽  
1998 ◽  
Vol 17 (4) ◽  
pp. 377-382 ◽  
Author(s):  
A. Winter ◽  
R. S. Appeldoorn ◽  
A. Bruckner ◽  
E. H. Williams Jr. ◽  
C. Goenaga
Keyword(s):  
Puerto Rico ◽  
Coral Reef ◽  
Caribbean Sea ◽  
Sea Surface ◽  
Sea Surface Temperatures ◽  
Surface Temperatures ◽  
La Parguera
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