Meyer, A2010-09-022010-09-022010-09-01Meyer, A. 2010. Impact of climate change on large scale coastal currents of South Africa. CSIR 3rd Biennial Conference 2010. Science Real and Relevant. CSIR International Convention Centre, Pretoria, South Africa, 30 August – 01 September 2010, pp 1http://hdl.handle.net/10204/4294CSIR 3rd Biennial Conference 2010. Science Real and Relevant. CSIR International Convention Centre, Pretoria, South Africa, 30 August – 01 September 2010The increase in equatorial temperatures and the presence of an ozone hole over Antarctica have caused an increase in the pole-to-equator pressure gradient with a concomitant intensification of the high-latitude westerlies (Cai et al., 2006). The transfer of momentum from the westerlies to the underlying Antarctic Circumpolar Current (ACC ) (Figure 1) has lead to a steady increase in ACC velocity. Since this current is in contact with the southern boundaries of the Southern Hemisphere subtropical gyre systems, a spinning up and southward shift of these basin scale gyres have been observed.enClimate changeCoastal areasCSIR Conference 2010Impact of climate change on large scale coastal currents of South AfricaConference PresentationMeyer, A. (2010). Impact of climate change on large scale coastal currents of South Africa. CSIR. http://hdl.handle.net/10204/4294Meyer, A. "Impact of climate change on large scale coastal currents of South Africa." (2010): http://hdl.handle.net/10204/4294Meyer A, Impact of climate change on large scale coastal currents of South Africa; CSIR; 2010. http://hdl.handle.net/10204/4294 .TY - Conference Presentation AU - Meyer, A AB - The increase in equatorial temperatures and the presence of an ozone hole over Antarctica have caused an increase in the pole-to-equator pressure gradient with a concomitant intensification of the high-latitude westerlies (Cai et al., 2006). The transfer of momentum from the westerlies to the underlying Antarctic Circumpolar Current (ACC ) (Figure 1) has lead to a steady increase in ACC velocity. Since this current is in contact with the southern boundaries of the Southern Hemisphere subtropical gyre systems, a spinning up and southward shift of these basin scale gyres have been observed. DA - 2010-09-01 DB - ResearchSpace DP - CSIR KW - Climate change KW - Coastal areas KW - CSIR Conference 2010 LK - https://researchspace.csir.co.za PY - 2010 T1 - Impact of climate change on large scale coastal currents of South Africa TI - Impact of climate change on large scale coastal currents of South Africa UR - http://hdl.handle.net/10204/4294 ER -