4. Applying the Framework: Comparative Analysis of Climate Security Dimensions
Having developed the multidimensional framework in
Section 3, this section applies it to substantive empirical terrain, examining how each dimension manifests across concrete cases of interstate and intrastate climate security dynamics. The analysis proceeds dimension by dimension, beginning with resource competition and transboundary water governance (
Section 4.1) and climate-induced migration and regional instability (
Section 4.2), before turning to territorial change in small island states and the Arctic (
Section 4.3). It then examines food security and political stability (
Section 4.4), cooperation opportunities and environmental peacebuilding (
Section 4.5), securitization dynamics and the climatization of security (
Section 4.6), and infrastructure vulnerability and cascading risks (
Section 4.7). Read together, these cases illustrate both the explanatory reach of the framework and the ways its seven dimensions interact in practice, setting up the theoretical and policy implications developed in
Section 5.
4.1. Resource Competition and Transboundary Water Governance
Water scarcity and agricultural stress represent perhaps the most extensively studied dimensions of climate security. Approximately 40% of the world's population lives in river basins shared by two or more countries, and climate change is altering hydrological patterns in ways that affect water availability, quality, and timing (UN-Water, 2018). Contrary to popular predictions of "water wars," historical analysis reveals that states have generally managed transboundary water disputes through cooperation rather than violent conflict. Wolf's research program documented more than 3,600 treaties governing international waters since 1820, with only a handful of militarized disputes directly attributable to water (Wolf, 2007). The Indus Waters Treaty between India and Pakistan, signed in 1960 and brokered by the World Bank, has survived three wars and persistent hostility between the signatories, demonstrating the resilience of institutionalized water cooperation (Zawahri, 2009). This cooperative record is consistent with meta-analytic findings that resource scarcity translates into conflict only under specific configurations of governance failure and distributional inequity rather than as a general rule (Vesco et al., 2020).
Yet this cooperative pattern faces significant pressure from intensifying climate impacts. Changes in glacial melt, monsoon behavior, and precipitation variability are altering the hydrological assumptions on which existing agreements were built (Zeitoun et al., 2013). The Nile Basin illustrates these tensions, with the Grand Ethiopian Renaissance Dam creating friction among Ethiopia, Sudan, and Egypt over allocation in a basin already stressed by population growth and climate variability (Tawfik, 2016). The Mekong Basin faces similar pressures, as upstream dam construction and climate-induced changes in flow affect downstream fisheries and agriculture (Matthews & Motta, 2015). How governments frame these pressures matters as well: in the Middle East and North Africa, official climate-security discourses often emphasize water and food risks to regime stability while sidelining the livelihood and rights dimensions that shape long-term resilience (Daoudy et al., 2022).
Table 4 profiles selected transboundary agreements and their capacity to accommodate climate adaptation.
The analytical lesson from transboundary water governance is that institutional arrangements matter decisively in determining whether resource pressures generate conflict or cooperation. Well-designed agreements with flexible allocation mechanisms, monitoring systems, and dispute-resolution procedures can absorb significant climate stress, while brittle arrangements or absent institutions leave states vulnerable to escalation (Dinar, 2011). Water governance also illustrates the peacebuilding mechanisms specified by Krampe et al. (2021): basin institutions create sustained intergroup contact, enhance state legitimacy through service delivery, and deepen interdependence in ways that raise the cost of conflict. This suggests that climate adaptation in transboundary basins requires not merely technical infrastructure but institutional innovation capable of managing uncertainty and distributing adaptation burdens equitably.
4.2. Climate-Induced Migration and Regional Instability
Climate migration has become one of the most prominent and politically charged dimensions of the climate–security nexus, generating alarming projections and intense policy debate (McLeman, 2014). The World Bank's Groundswell modeling projects that, absent effective climate action, up to 216 million people could be displaced within their own countries by 2050 across six regions (Clement et al., 2021). The demographic stakes are underscored by research on the human climate niche, which estimates that each additional degree of warming above present levels could leave hundreds of millions of people outside the climatic conditions that have historically sustained dense human settlement (Lenton et al., 2023). Most climate-related movement is expected to be internal rather than cross-border, challenging common assumptions in security discourse; even internal displacement, however, can generate international implications through spillover effects, humanitarian pressures, and political destabilization. As shown in
Figure 3, projected displacement is heavily concentrated in Sub-Saharan Africa, East Asia and the Pacific, and South Asia—regions where adaptive capacity is most constrained (
Figure 3).
The relationship between climate migration and interstate conflict is complex and contested. Some scholars argue that climate migration can exacerbate tensions in receiving areas, particularly where resource competition, ethnic divisions, or political fragility already exist (Reuveny, 2007). Others emphasize that migration often functions as an adaptive response that reduces pressure in origin areas, with security implications depending heavily on political management (Black et al., 2011). Meta-analytic evidence clarifies this heterogeneity: across 30 country-level studies, environmental change increases migration primarily at middle income levels and through livelihood channels, whereas the poorest populations are frequently
trapped rather than mobile (Hoffmann et al., 2020)—a finding that complicates alarmist projections and underscores the mediated character of migration outcomes. Crucially, the climate–migration–conflict chain appears to operate only under restrictive conditions: analyzing global asylum flows, Abel et al. (2019) find that climatic conditions influenced cross-border displacement only during specific periods and in countries undergoing political transformation, with drought severity raising the likelihood of armed conflict that in turn drove refugee movements. The Syrian conflict has been invoked as a putative case of climate-induced instability, with the 2006–2010 drought contributing to rural–urban migration before the 2011 uprising, though causal claims remain sharply contested (Kelley et al., 2015; Selby et al., 2017).
Table 5 details the regional projections and their principal drivers.
International legal frameworks remain poorly adapted to climate-induced displacement. The 1951 Refugee Convention does not recognize environmental factors as grounds for refugee status, creating a protection gap for those displaced by climate impacts (McAdam, 2012). The Nansen Initiative and its successor, the Platform on Disaster Displacement, have advanced soft-law frameworks for cross-border climate displacement, but binding international instruments remain elusive (Kälin, 2015). This legal ambiguity itself generates security tensions as states navigate competing obligations and political pressures in managing climate-related population movements.
4.3. Territorial Change: Small Island States and Arctic Geopolitics
Climate change poses existential challenges to territorial integrity that international law and international relations theory are ill-equipped to address. Rising sea levels threaten the physical existence of small island states, while the opening of Arctic shipping routes creates new theaters of geopolitical competition. Both phenomena raise fundamental questions about sovereignty, territory, and international order.
4.3.1. Disappearing States
Small island developing states including Tuvalu, Kiribati, the Maldives, and the Marshall Islands face potential loss of territory from sea-level rise (McAdam, 2012). Projected rise of 0.28–1.01 meters by 2100 under different emissions scenarios would render portions of these states uninhabitable well before complete submergence, through salinization of freshwater aquifers, destruction of agricultural land, and increased storm-surge vulnerability (IPCC, 2021). The implications for statehood are profound and largely unresolved. Under the Montevideo Convention (1933), statehood requires a permanent population, defined territory, government, and capacity for international relations; potential loss of territory and population raises questions about whether affected states would continue to exist under international law (Wong, 2013). Emerging proposals include "deterritorialized states" retaining sovereign status despite territorial loss, ex-situ governments maintaining institutional continuity from territory provided by other states, and novel sovereign arrangements adapted to climate realities (Burkett, 2011). Maritime entitlements under the UN Convention on the Law of the Sea present additional complications, since exclusive economic zones are measured from baselines that could retreat with coastlines; the Pacific Islands Forum declared in 2021 that member states would maintain existing maritime zones regardless of climate-induced sea-level change, challenging conventional interpretations of maritime law (Pacific Islands Forum, 2021).
4.3.2. Arctic Geopolitics
The Arctic represents perhaps the most dramatic case of climate-induced geopolitical change. Sea-ice extent has declined markedly since 1979—with reductions across all seasons—opening shipping routes and creating access to previously inaccessible resources (Stroeve & Notz, 2018). The Northern Sea Route and Northwest Passage can substantially cut shipping distances between Europe and Asia, and the region is estimated to hold about 13% of undiscovered global oil and 30% of undiscovered gas (USGS, 2008). These changes have intensified competition among the eight Arctic states and attracted non-Arctic powers, including China, which has declared itself a "near-Arctic state." Russian military modernization—including the reopening of Soviet-era bases—has heightened concern about the region's strategic trajectory, and Russia's 2022 invasion of Ukraine disrupted Arctic governance, with the Arctic Council suspending cooperation involving Russia (Conley et al., 2020). Assessing this rupture, Koivurova and Shibata (2023) conclude that while functional cooperation on science, search and rescue, and fisheries may be partially sustainable, the invasion has damaged the institutional trust on which three decades of "Arctic exceptionalism" retain instructive demonstration that climate-driven cooperation remains hostage to broader geopolitical shocks.
Table 6 summarizes the principal sovereignty claims and disputes.
Despite increased tension, Arctic governance has historically demonstrated substantial cooperation through the Arctic Council and related institutions. The Ilulissat Declaration (2008) affirmed commitment to the law of the sea as the framework for resolving Arctic disputes, and the region has produced binding agreements on search and rescue, oil-spill response, and scientific cooperation (Byers, 2013). Whether this cooperative pattern survives intensifying great-power competition remains a critical question for Arctic security—and a revealing test of the contingency thesis advanced in this paper.
4.4. Food Security and Political Stability
Climate change is transforming global food systems in ways that carry significant implications for political stability and interstate relations. Agricultural productivity in many regions is projected to decline due to heat stress, water scarcity, and changing precipitation, while extreme weather increasingly disrupts production and distribution; the IPCC concludes with high confidence that climate change has already affected food security in the most vulnerable regions (IPCC, 2022). Food price volatility represents a particularly potent political risk. The 2007–2008 and 2010–2011 price spikes, partly attributable to climate-related production shortfalls, contributed to unrest in numerous countries, including those affected by the Arab Spring uprisings (Bellemare, 2015; Werrell & Femia, 2013). Micro-level evidence corroborates this pathway: analyzing millions of geolocated social media messages, Koren et al. (2021) show that localized experiences of food and water insecurity significantly raise the probability of protest and unrest, providing granular support for the aggregate price–instability relationship. The relationship between food prices and instability is mediated by government response capacity, import dependence, and social safety nets, but the potential for climate-induced food shocks to trigger crises with international reverberations is well documented.
Trade conflicts over agricultural resources constitute another pathway through which food security affects interstate relations. Export restrictions imposed during supply crises amplify global price volatility and generate diplomatic tension, as when major exporters restricted grain exports during the 2007–2008 crisis (Headey & Fan, 2010). More recently, the Russia–Ukraine war's disruption of grain and fertilizer exports illustrated how conflicts in major agricultural regions generate global food-security crises with cascading political effects: because Russia and Ukraine jointly supplied roughly one-tenth of globally traded calories, import-dependent states across the Middle East and Africa faced acute exposure to a shock originating far beyond their borders (Hellegers, 2022). Longer term, warming may reconfigure global agricultural geography, shifting production toward higher latitudes as tropical and subtropical productivity declines—a restructuring that could generate new patterns of strategic dependence for food-importing regions in the Middle East, North Africa, and parts of Asia (Wheeler & von Braun, 2013).
4.5. Cooperation Opportunities and Environmental Peacebuilding
Analysis of climate cooperation as a confidence-building measure contributes to understanding environmental peacemaking—how shared environmental challenges create opportunities for diplomatic engagement even among adversaries. The environmental peacebuilding literature identifies multiple pathways through which environmental cooperation can contribute to broader peace: building trust through technical cooperation, creating institutional frameworks for communication, addressing underlying grievances, and generating shared benefits that strengthen cooperative constituencies (Conca & Dabelko, 2002; Ide, 2019; Krampe et al., 2021). Empirically, Ide (2018) finds that cooperative environmental agreements have measurably contributed to reconciliation in several international rivalries, though effects are conditional on political context.
Table 7 summarizes the principal mechanisms with illustrative cases and effectiveness conditions.
Climate cooperation offers particularly promising avenues for peacebuilding because climate change is a genuinely shared global challenge that cannot be addressed unilaterally. The Paris Agreement's framework of nationally determined contributions, collective stocktaking, and enhanced transparency creates structured opportunities for engagement among states with otherwise divergent interests (Falkner, 2016), while climate finance, technology transfer, and adaptation cooperation create material stakes in cooperative relationships that can buffer political tension. The Environment of Peace assessment reaches a parallel conclusion at the level of grand strategy: because environmental degradation and insecurity now compound one another, investments in cooperative environmental governance function simultaneously as instruments of peace and of risk reduction (Black et al., 2022). However, environmental peacebuilding faces significant limitations. Selection bias may overstate success, as failed cooperation receives less scholarly attention than visible successes; cooperation can reinforce power asymmetries when inattentive to equity; and technical cooperation may substitute for, rather than enable, political engagement on harder issues (Ide, 2020). Climate cooperation specifically confronts the collective-action problems of global public goods, distributional conflict over emission reductions, and the vulnerability of multilateral frameworks to great-power competition (Colgan et al., 2021).
4.6. Securitization Dynamics and the Climatization of Security
The securitization of climate change has proceeded unevenly across states, institutions, and issue areas, with significant implications for both security and climate governance. The Copenhagen School analyzes securitization as a speech act through which issues are constructed as existential threats requiring extraordinary measures (Buzan et al., 1998). Climate change presents an ambiguous case, combining features of successful securitization—widespread acknowledgment as a major threat, institutional response—with clear limits, notably the absence of emergency measures commensurate with the identified threat (Oels, 2012; Trombetta, 2008). Three modes of climate securitization can be distinguished analytically: risk-based securitization, which connects climate to established risk-management practices; humanitarian securitization, which centers vulnerable populations as referent objects; and militarized securitization, which emphasizes traditional security implications with corresponding defense and intelligence responses (Methmann & Rothe, 2012; von Lucke et al., 2014). A fourth, ecological mode—centered on Earth systems and planetary boundaries—has gained prominence in recent discourse. Comparative research demonstrates that these framings are not merely rhetorical: which mode prevails shapes whose security is prioritized and which policy instruments become thinkable, as studies of climate-security discourse in the Middle East and North Africa illustrate (Daoudy et al., 2022).
Table 8 compares these modes and their policy implications.
Critical scholars identify several risks in climate securitization. Militarization may displace civilian expertise and development-oriented approaches (Hardt, 2018); security framing may construct climate-vulnerable populations as threats rather than victims, legitimizing restrictive rather than supportive policies (Bettini, 2013); and the emergency logic of security may be incompatible with the long-term structural transformation effective climate response requires (Methmann & Rothe, 2012). Balancing the mobilizational power of security framings against these risks remains an ongoing analytical and political challenge.
4.7. Infrastructure Vulnerability and Cascading Risks
The final dimension addresses infrastructure vulnerability to climate-driven disasters, which creates cascading risks with significant international implications. Critical infrastructure—energy systems, transportation networks, water supplies, communications—faces increasing exposure to extreme weather and sea-level rise, with damage in Europe alone projected to increase tenfold by century's end under high-emissions scenarios (Forzieri et al., 2018). Infrastructure failures generate cascade effects across interconnected systems and international boundaries, ranging from economic disruption to humanitarian crisis and political destabilization. Globalization has intensified these interdependencies: supply chains spanning multiple jurisdictions can be disrupted by localized disasters with global consequences, as the 2011 Thailand floods demonstrated when a national disaster disrupted global hard-drive and automotive manufacturing (Haraguchi & Lall, 2015). Such compounding, transboundary dynamics exemplify the systemic risks that increasingly characterize a densely interconnected world (Renn et al., 2019). Climate adaptation of critical infrastructure requires substantial investment—the OECD estimates USD 6.9 trillion annually in infrastructure investment through 2030 to meet climate and development objectives (OECD, 2018)—and international cooperation on standards, financing, and emergency response remains an underdeveloped dimension of climate security governance.