Figure 1: Arctic Temperature Trends

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Climate Change in the Arctic and its Implications for U.S. National Security Elizabeth L. (Fletcher PhD candidate) IDEAS, April 2007, http://fletcher.tufts.edu/ierp/ideas/default.html The Arctic, viewed as a place of ice floes and polar bears, will be the earth s first laboratory of climate change, which will affect oil and gas removal, allow increased ocean access, and raise resurgent legal concerns. These effects make this area worthy of consideration for long-range U.S. policy formation and merit bringing the Arctic back into prominence in American strategic thinking. Anthropogenic Greenhouse Warming in the Arctic Greenhouse warming in the Arctic, as shown in Figure 1, will have three significant positive feedback loops not felt elsewhere on the globe. First, the warming potential of the Arctic is more significant than the rest of the globe because snow and ice melt will change local albedo levels from high to low. As highly reflective snow and ice cover melt into highly absorptive water, surface area that used to reflect sunlight will now absorb it, radiating the resulting energy back from the earth as heat. Second, since the planetary atmosphere is shallower toward the poles, the volume of air that must be warmed in order for the surface to begin warming is less. Third, as sea ice retreats, heat that is absorbed by the oceans in the summer is readily transferred to the atmosphere in winter. Since much of the Arctic s environment is close to 32º F, a relatively small increase in the ambient air temperature can result in large environmental changes and feedbacks. Two 2007 findings from the IPCC have indicated that average Arctic temperatures increased at almost twice the global average rate in the past 100 years. Annual average Arctic sea ice extent, the area of ocean that is covered by at least 15 percent ice, has shrunk by 2.7 percent per decade since 1978, while permafrost temperature has increased. These temperature changes are likely to lead to reductions in thickness and size of glaciers and ice sheets, and reductions in extent of sea ice and permafrost. In November of 2004, the Arctic Council published a summary of their two-year assessment of the impact of climate change in the Arctic, the Arctic Climate Impact Assessment (ACIA). The results were alarming beyond even the IPCC s predictions. While regional variations exist, the evidence shows a clear and significant warming trend across most of the Arctic. Up from an observed temperature increase of 5 to 7º F over the past fifty years, the ACIA predicts an increase in ambient air temperatures of 5 to 9º F over land and up to 13º F over the ocean within the next 100 years. Wintertime averages over land and sea for the same period will increase 7 to 13º F and 13 to 18º F, respectively. Page 1 of 6

Figure 1: Arctic Temperature Trends (graphic: NASA Earth Observatory; the black area at the North Pole represents gaps in data coverage.) Significant climate change in the Arctic will result in both increasing loss of sea ice cover, and thinning ice. Over the past thirty years, annual average sea ice cover has declined by 8 percent. Additional declines in average annual sea ice cover have been predicted at 10 to 50 percent. However, the most recent computer models from the American Geographic Union speculate that gradual ice thinning will give way to sudden ice loss, rendering the summer Arctic virtually ice-free by 2040 (Figure 2). This is decades earlier that previously predicted. Concomitantly, the trend in sea-level rise is also accelerating. Global average sea level has risen approximately three inches in the past thirty years due to thermal expansion and melting of land-based ice. In this century, global average sea level is predicted to rise between four inches and three feet, with the rate of rise increasing toward the end of the century. Finally, changes in thermohaline circulation may flow from increasing Arctic ice melt. The ocean is a delicate balance of salt and fresh water, sometimes referred to as the Great Ocean Conveyor in which specific currents carry warm and cold water around the globe. Added freshwater runoff from melting glaciers may alter or shut down this circulation, resulting in widespread regional climatic changes such as colder European winters and changing fish migration patterns. Page 2 of 6

Figure 2: Projected Extent of Sea Ice Melting (graphic: New York Times 2006) Oil & Gas Infrastructure One energy security challenge the United States and all circumpolar nations will face is the viability of oil and gas infrastructure in the far north. The Arctic contains as much as 40 percent of world oil and gas reserves. Siberia alone is estimated to hold petroleum reserves equal to the Middle East. Climate change will make petroleum extraction easier and more economical by allowing regular sea transport over newly ice-free sea lanes. Once on land, however, the burning of these same fossil fuels will make it that much more difficult to get at the hydrocarbons in the Arctic. Existing pumps, pipelines, infrastructure buildings, and workers housing are built on permafrost. Since the bearing capacity of permafrost decreases with warming, the land will subside considerably when it thaws, resulting in shifting ground, erosion, landslides, and land subsidence. Structural damage will reduce oil companies ability to extract oil economically by forcing them to sink additional costs into infrastructure preservation and operation. A stoppage of North Slope oil will imperil U.S. energy security by foreshortening the supply and forcing the United States to either conserve oil, a politically unpopular choice for the current administration, or import the shortfall from other nations. If the United States chooses to do so from the Middle East, American soldiers face extended tours of duty in Iraq, Saudi Arabia, and other oil-producing countries in the region. Page 3 of 6

Increased Arctic Ocean Access An open-water Arctic is a more accessible Arctic for the international community. Naval vessels, merchant ships, recreational boats, cruise liners, and especially submarines will find an accessible Arctic to their advantage. However, while an ice-free Arctic may translate into more trade and material wealth, increased ship traffic will also result in a rising number of vessels from hostile nations or non-state actors, who have no incentive to obey internationally-accepted laws regarding national waters or even notify a country of their presence. This will require the United States to enlarge its military presence in the Arctic to monitor shipping and military traffic through its adjacent waters. Complicating the access issue are Canada s claims of territoriality. In 1977, Canada declared the Northwest Passage to be Canadian internal waters. The issue has not yet been tested either in court or by show of Canadian force. Interestingly, legal scholars have not supported this position explicitly, though the Arctic has been frozen over and the Northwest Passage impassable for most of the year, so the issue has been functionally moot. However, as climate change melts the Arctic ice, more surface ship traffic will force the Canadians to either defend their claim or abandon it. This situation may strain the relationship with the United States if the Americans, concerned about increasing traffic to the north, think that Canada cannot adequately patrol its Arctic waters. The Northeast Passage, also called the Northern Sea Route, will also become ice-free for a greater part of the year, and the United States will certainly try to take advantage of that new mobility. Russia, therefore, will find itself in the same position as Canada with regard to its territorial waters, although they have a much more ice-capable navy and have indicated an interest in allowing transit through the Passage for commercial ships. New Missions and Operational Capabilities Naval Arctic missions for the United States in a globally-warmed world would result as a response to security challenges from hostile nations or from opportunities to exploit operational efficiencies offered by peacetime Arctic transit. The U.S. Office of Naval Research (ONR) has identified the nine most likely missions that the United States would face in an ice-free Arctic: 1. law enforcement operations; 2. ensure freedom of navigation; 3. protection of natural resources; 4. transit of forces; 5. homeland defense; 6. forward presence, intelligence, surveillance and reconnaissance (ISR); 7. scientific exploration; 8. maintain/improve capability to operate in the Arctic; 9. uphold allied commitments. More specifically, the United States might face Russian naval incursions into its northern waters. Although these two countries are currently allies, American (and Canadian) strategic considerations would not permit Russia to have unfettered access to the Western Hemisphere Arctic. Page 4 of 6

Policy Recommendations RECOMMENDATION 1: TRAIN AND EQUIP THE U.S. MILITARY FOR ARCTIC OPERABILITY. To be able to execute these new missions and see to its Northern defense, the United States will need to start planning for Arctic operability now. Currently, the U.S. Coast Guard has only two aging icebreakers, while the U.S. Navy has none. U.S. naval ships would have to be ice-strengthened, soldiers, and sailors would have to be Arctic-trained, and weaponry and machinery would need to be built to withstand Arctic conditions if the United States are to maintain a consistent and capable presence in the far North. In addition, the United States will need to invest time, money, and goodwill in bilateral and multilateral alliances in the region to maximize its efficiency in the area. Military experts have suggested fruitful grounds for cooperation, such as a joint U.S-Canadian Arctic search and rescue operation. RECOMMENDATION 2: INCREASE FUNDING FOR EARTH MONITORING SATELLITES AND DATA COLLECTION. A recent report from the National Research Council states that the number of earthobserving instruments will drop to 60 percent of current capacity by 2010, a victim of both under-funding and the administration s call to focus on manned space missions (http://www.nap.edu/catalog/11820.html). This policy decision is severely misguided. Earth-based data collection is the backbone not only of our climate prediction capability but also of our ability to understand and respond to environmentally-generated threats. Scientists and policy makers can only make an educated guess at the likelihood and severity of these threats. Yet if they are significant enough, they can overwhelm society s adaptive capacity and leave all United States plans for strategic superiority in the dust. However, an uncertain timeline of effects is not necessarily fatal to consideration of adaptive measures. It would be strategically short-sighted to insist upon waiting for climate models to specify exact effects and locations. Rather, the identified trends provide enough information for forward-thinking nations to begin building operational flexibility into their defenses that would allow for adaptability to future conditions. RECOMMENDATION 3: INCREASE DIPLOMATIC, MILITARY, AND SCIENTIFIC COOPERATION WITH OTHER CIRCUMPOLAR NATIONS. Some scholars posit that ongoing environmental change in the Arctic is one of the clearest indicators of the need for new geopolitical thinking. Multinational organizations such as the Arctic Council have gone a long way towards bringing the scientific realities of the Arctic to the attention of policymakers around the northern hemisphere. Franklyn Griffiths, a well-known Canadian Arctic scholar, argues that international scientific collaboration can help reinforce military cooperation in the area. This collaboration is all the more pressing given new discoveries of the effects of climate change on the polar environment. The creation of a new defense institution might help to further international security in the Arctic in the face of ecological and economic changes brought about by global warming. A permanent standing bilateral body (not unlike the International Joint Page 5 of 6

Commission that oversees the Great Lakes and other U.S.-Canadian boundary waters) could institutionalize the Far North as an area of legitimate joint concern. Staffed with Arctic experts and possessing its own budget, it could ensure that Arctic matters were high in the pantheon of defense concerns we face. In a bold move, a trilateral institution could include Russia, thus ensuring that the major Arctic powers had a forum to resolve access disputes and to discuss and act upon security concerns in concert. Conclusion Security planners and policy makers tend to believe that the future will resemble the past. We assume that the important problems of the day will remain important into the future and our policy planning reflects this. However, the predicted Arctic melt will thrust policy makers and planners into a world that has literally never existed before. If the models that predict an ice-free Arctic by 2040 are correct, the United States must embrace the concept of environmental security especially as it applies in the Arctic, the first laboratory of global climate change if it is to remain secure. The empirical evidence of global warming is one of the clearest indications that circumpolar nations need to change their strategic and geopolitical thinking, from the solely military viewpoint to one that includes military, environmental, economic, and human aspects. Already Inuit peoples have discovered commonalities with Pacific Islanders as they see themselves as victims of diminished adaptive capacity with their homes and traditional ways of life eroded by climate change. The United States, a wealthy country with a robust adaptive capacity, may yet see its way of life erode if it does not respect the links between climate and national security. Center for International Environmental and Resource Policy The Fletcher School Tufts University Page 6 of 6