Aquatic Environment and Biodiversity Annual Review 2012
Aquatic Environment and Biodiversity Annual Review 2012 Aquatic Environment and Biodiversity Annual Review 2012
AEBAR 2012: Ecosystem effects: NZ regional climate and oceanic setting 8.1. Context which is likely to result in fewer El Niño events for a 20–30 year period, i.e., less zonal westerly winds (already apparent compared to the 1980– 2000 period) and increased temperatures; this is the first regime shift to occur since most of our fisheries monitoring time series have started (the previous shift was in the late 1970s), and will likely impact on fish productivity • New Zealand trends of increasing air and sea temperatures and ocean acidification are consistent with global trends. Climate and oceanographic conditions play an important role in driving the productivity of our oceans and the abundance and distribution of our fishstocks, and hence fisheries. A full analysis of trends in climate and oceanographic variables in New Zealand is given in Hurst et al. (2012) and is now being developed as an Ocean Climate Change Atlas for New Zealand waters (Boyd and Law.2011). New Zealand is essentially part of a large submerged continent (Figure 8.1). Figure 8.1: New Zealand land mass area 250,000 km 2 ; EEZ & territorial sea area (pink) 4,200,000 km 2 ; extended continental shelf extension area (light green) 1,700,000 km 2 ; Total area of marine jurisdiction 5,900,000 km 2 . The black line shows the boundary of the New Zealand EEZ, the yellow line indicates the extension to New Zealand’s legal continental shelf, and the red line the agreed Australia/New Zealand boundary under UNCLOS Article 76. Image courtesy of GNS. The territorial sea (TS extending from mean low water shore line to 12 nautical miles) and Exclusive Economic Zone (the EEZ, extending from 12 nautical miles to 200 miles offshore) and the extended continental shelf (ECS) combine to produce one of the largest areas of marine jurisdiction in the world, an area of almost 6 million square kilometres, (Figure 8.1). New Zealand waters straddle more than 25 degrees of latitude from 30º S in warm subtropical waters to 56º S in cooler, subantarctic 189
AEBAR 2012: Ecosystem effects: NZ regional climate and oceanic setting waters, and 28 degrees of longitude from 161º E in the Tasman Sea to 171º W in the west Pacific Ocean. New Zealand’s coastline, with its numerous embayments, is also long, with estimates ranging from 15,000 to 18,000 km, depending on the method used for measurement (Gordon et al. 2010). New Zealand lies across an active subduction zone in the western Pacific plate, tectonic activity and volcanism have resulted in a diverse and varied seascape within the EEZ. The undersea topography comprises a relatively narrow band of continental shelf down to 200 m water depth, extensive continental slope areas from 200 to 1000 m, extensive abyssal plains, submarine canyons and deep sea trenches, ridge systems and numerous seamounts and other underwater topographic features such as hills and knolls. There are three significant submarine plateaus, the Challenger Plateau, the Campbell Plateau in the subantarctic, and the Chatham Rise (Figure 8.2). Disturbance of current flow across the plateaus and around the New Zealand landmass gives rise to higher ocean productivity than might be expected, given New Zealand’s isolated location in the generally oligotrophic western Pacific Ocean (Figure 8.3). Higher ocean colour, reflecting higher levels of productivity, is typically found around the coast and to the east across the Chatham Rise (Figure 8.3; Pinkerton et al. 2005). The coastal waters and plateaus support a range of commercial shellfish and finfish fisheries from the shoreline to depths of about 1500 m. Seamounts, seamount chains and ridge structures in suitable depths provide additional localized areas of upwelling and increased productivity sometimes associated with commercial fisheries. Figure 8.2 Undersea topography of New Zealand (red shallow to blue deep). White dash line shows the EEZ boundary. Image courtesy of NIWA. . 190
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AEBAR <strong>2012</strong>: Ecosystem effects: NZ regional climate <strong>and</strong> oceanic setting<br />
8.1. Context<br />
which is likely to result in fewer El Niño events for a 20–30 year period,<br />
i.e., less zonal westerly winds (already apparent compared to the 1980–<br />
2000 period) <strong>and</strong> increased temperatures; this is the first regime shift to<br />
occur since most of our fisheries monitoring time series have started (the<br />
previous shift was in the late 1970s), <strong>and</strong> will likely impact on fish<br />
productivity<br />
• New Zeal<strong>and</strong> trends of increasing air <strong>and</strong> sea temperatures <strong>and</strong> ocean<br />
acidification are consistent with global trends.<br />
Climate <strong>and</strong> oceanographic conditions play an important role in driving the productivity of our oceans<br />
<strong>and</strong> the abundance <strong>and</strong> distribution of our fishstocks, <strong>and</strong> hence fisheries. A full analysis of trends in<br />
climate <strong>and</strong> oceanographic variables in New Zeal<strong>and</strong> is given in Hurst et al. (<strong>2012</strong>) <strong>and</strong> is now being<br />
developed as an Ocean Climate Change Atlas for New Zeal<strong>and</strong> waters (Boyd <strong>and</strong> Law.2011).<br />
New Zeal<strong>and</strong> is essentially part of a large submerged continent (Figure 8.1).<br />
Figure 8.1: New Zeal<strong>and</strong> l<strong>and</strong> mass area 250,000 km 2 ; EEZ & territorial sea area (pink) 4,200,000 km 2 ; extended<br />
continental shelf extension area (light green) 1,700,000 km 2 ; Total area of marine jurisdiction 5,900,000 km 2 . The<br />
black line shows the boundary of the New Zeal<strong>and</strong> EEZ, the yellow line indicates the extension to New Zeal<strong>and</strong>’s<br />
legal continental shelf, <strong>and</strong> the red line the agreed Australia/New Zeal<strong>and</strong> boundary under UNCLOS Article 76.<br />
Image courtesy of GNS.<br />
The territorial sea (TS extending from mean low water shore line to 12 nautical miles) <strong>and</strong> Exclusive<br />
Economic Zone (the EEZ, extending from 12 nautical miles to 200 miles offshore) <strong>and</strong> the extended<br />
continental shelf (ECS) combine to produce one of the largest areas of marine jurisdiction in the<br />
world, an area of almost 6 million square kilometres, (Figure 8.1). New Zeal<strong>and</strong> waters straddle more<br />
than 25 degrees of latitude from 30º S in warm subtropical waters to 56º S in cooler, subantarctic<br />
189