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NMFS Biological Opinion on U.S. Navy training ... - Govsupport.us

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FINAL PROGRAMMATIC BIOLOGICAL OPINION ON U.S. NAVY ACTIVITIES IN THE HAWAII RANGE COMPLEX 2008-2013<br />

affect the distributi<strong>on</strong> of cephalopod populati<strong>on</strong>s, but would not reduce the number or density of cephalopod<br />

populati<strong>on</strong>s. If, however, cephalopod populati<strong>on</strong>s collapse or decline dramatically, sperm whale populati<strong>on</strong>s are<br />

likely to collapse or decline dramatically as well.<br />

The resp<strong>on</strong>se of North Atlantic right whales to changes in the North Atlantic Oscillati<strong>on</strong> also provides insight into<br />

the potential c<strong>on</strong>sequences of a changing climate <strong>on</strong> large whales. Changes in the climate of the North Atlantic have<br />

been directly linked to the North Atlantic Oscillati<strong>on</strong>, which results from variability in pressure differences between<br />

a low pressure system that lies over Iceland and a high pressure system that lies over the Azore Islands. As these<br />

pressure systems shift from east to west, they c<strong>on</strong>trol the strength of westerly winds and storm tracks across the<br />

North Atlantic Ocean. The North Atlantic Oscillati<strong>on</strong> Index, which is positive when both systems are str<strong>on</strong>g<br />

(producing increased differences in pressure that produce more and str<strong>on</strong>ger winter storms) and negative when both<br />

systems are weak (producing decreased differences in pressure resulting in fewer and weaker winter storms), varies<br />

from year to year, but also exhibits a tendency to remain in <strong>on</strong>e phase for intervals lasting several years.<br />

Sea surface temperatures in the North Atlantic Ocean are closely related to this Oscillati<strong>on</strong> and influences the<br />

abundance of marine mammal prey such as zooplankt<strong>on</strong> and fish. In the 1970s and 1980s, the North Atlantic<br />

Oscillati<strong>on</strong> Index have been positive and sea surface temperatures increased. These increased are believed to have<br />

produced c<strong>on</strong>diti<strong>on</strong>s that were favorable for the copepod (Calan<strong>us</strong> finmarchic<strong>us</strong>), which is the principal prey of<br />

North Atlantic right whales (C<strong>on</strong>versi et al. 2001) and may have increased calving rates of these whales (we cannot<br />

verify this associati<strong>on</strong> beca<strong>us</strong>e systematic data <strong>on</strong> North Atlantic right whale was not collected until 1982; Greene et<br />

al. 2003). In the late 1980s and 1990s, the NAO Index was mainly positive but exhibited two substantial, multi-year<br />

reversals to negative values. This was followed by two major, multi-year declines in copepod prey abundance<br />

(Pershing et al. 2001, Drinkwater et al. 2003). Calving rates for North Atlantic right whales followed the declining<br />

trend in copepod abundance, although there was a time lag between the two (Greene et al. 2003).<br />

Although the NAO Index has been positive for the past 25 years, atmospheric models suggest that increases in ocean<br />

temperature associated with climate change forecasts may produce more severe fluctuati<strong>on</strong>s in the North Atlantic<br />

Oscillati<strong>on</strong>. Such fluctuati<strong>on</strong>s would be expected to ca<strong>us</strong>e dramatic shifts in the reproductive rate of critically<br />

endangered North Atlantic right whales (Drinkwater et al. 2003; Greene et al. 2003) and possibly a northward shift<br />

in the locati<strong>on</strong> of right whale calving areas (Kenney 2007).<br />

Changes in global climatic patterns are also projected to have profound effect <strong>on</strong> the coastlines of every c<strong>on</strong>tinent by<br />

increasing sea levels and increasing the intensity, if not the frequency, of hurricanes and tropical storms. Based <strong>on</strong><br />

computer models, these phenomena would inundate nesting beaches of sea turtles, change patterns of coastal erosi<strong>on</strong><br />

and sand accreti<strong>on</strong> that are necessary to maintain those beaches, and would increase the number of turtle nests that<br />

are destroyed by tropical storms and hurricanes. Further, the combinati<strong>on</strong> of increasing sea levels, changes in<br />

patterns of coastal erosi<strong>on</strong> and accreti<strong>on</strong>, and changes in rainfall patterns are likely to affect coastal estuaries,<br />

submerged aquatic vegetati<strong>on</strong>, and reef ecosystems that provide foraging and rearing habitat for several species of<br />

sea turtles. Finally, changes in ocean currents associated with climate change projecti<strong>on</strong>s would affect the migratory<br />

patterns of sea turtles. The loss of nesting beaches, by itself, would have catastrophic effect <strong>on</strong> sea turtles<br />

populati<strong>on</strong>s globally if they are unable to col<strong>on</strong>ize any new beaches that form of if the beaches that form do not<br />

provide the sand depths, grain patterns, elevati<strong>on</strong>s above high tides, or temperature regimes necessary to allow turtle<br />

86

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