Natural and human systems of the Andes under climate change: local detection and attribution assessment of impacts in physical, biological and human systems

Author(s):  
Ana Ochoa-Sánchez ◽  
Fabian Drenkhan ◽  
Dáithí Stone ◽  
Daniel Mendoza ◽  
Ronald Gualán ◽  
...  

<p>Physical, biological, and human systems in mountain regions are highly sensitive to climate change due to strong feedbacks and low resilience. Detection of changes and attribution of them to climate and non-climate drivers provides ongoing monitoring of complex interactions of coupled natural and human systems and improving scientific assessments that inform mitigation and adaptation practices. In the IPCC 5<sup>th</sup> Assessment Report published in 2014, Central and South America was the region with the least evidence available for detection and attribution (D&A) of climate change impacts. Since then, much more evidence has accumulated due to an increasing number of studies detecting impacts in the Andean region. In this study, we therefore performed a systematic literature review of climate change impacts and made a local D&A expert impact assessment for a total of 12 natural and human systems in the Andes. We found the following confidence levels of detection and attribution of each impact for each system: medium and high, respectively, for energy; high and high, for snow and ice, tourism, and cultural values; high and medium for terrestrial and aquatic ecosystems, disasters, human health and migration; and medium and medium for agriculture and water systems. A total number of 65 sample impacts (in aggregate or case study form) could be attributed to climate change. Climate change was especially important in glacio-hydrological systems (49%) and terrestrial ecosystems (15%). Among the impacts that could be attributed to climate change with high confidence, snow and ice system dominated. About half of the total impact samples were attributed with medium confidence, of which 35% corresponded to water systems and 16% to agriculture. Finally, 14% of all impacts were assessed with low attribution confidence. Important results include: (1) glacier retreat leads to important cascading effects affecting most of the systems in the Andes; these impacts were primarily attributed to temperature increase caused by anthropogenic climate change; (2) numerous terrestrial and aquatic Andean ecosystems have been affected by climate change (e.g. upward plant colonization, changes in the abundance and distribution of species), and most of these impacts could be attributed to anthropogenic climate change; and (3) community changes and loss of cultural values are among the strongest impacts of human systems that were attributed to climate change; a broad set of studies detected that Andean communities perceived changes in their highly preserved long-standing cultural and spiritual rituals and cosmovision. These findings are key to understand current climate change impacts in the Andean region, and to advance our understanding of complex interactions of coupled natural and human systems in order to put particular attention on integrated scientific assessments and leverage local decision-making and management practices.</p>

2021 ◽  
Author(s):  
Christian Huggel ◽  
Simon K. Allen ◽  
Indra D. Bhatt ◽  
Rithodi Chakraborty ◽  
Fabian Drenkhan ◽  
...  

<p>Mountains cover about a quarter of the Earth’s land surface and are home to or serve a substantial fraction of the global population with essential ecosystem services, in particular water, food, energy, and recreation. While mountain systems are expected to be highly exposed to climate change, we currently lack a comprehensive global picture of the extent to which environmental and human systems in mountain regions have been affected by recent anthropogenic climate change.</p><p>Here we undertake an unprecedented effort to detect observed impacts of climate change in mountains regions across all continents. We follow the approach implemented in the IPCC 5<sup>th</sup> Assessment Report (AR5) and follow-up research where we consider whether a natural or human system has changed beyond its baseline behavior in the absence of climate change, and then attribute the observed change to different drivers, including anthropogenic climate change. We apply an extensive review of peer-reviewed and grey literature and identify more than 300 samples of impacts (aggregate and case studies). We show that a wide range of natural and human systems in mountains have been affected by climate change, including the cryosphere, the water cycle and water resources, terrestrial and aquatic ecosystems, energy production, infrastructure, agriculture, health, migration, tourism, community and cultural values and disasters. Our assessment documents that climate change impacts are observed in mountain regions on all continents. However, the explicit distinction of different drivers contributing to or determining an observed change is often highly challenging; particularly due to widespread data scarcity in mountain regions. In that context, we were also able to document a high amount of impacts in previously under-reported continents such as Africa and South America. In particular, we have been able to include a substantial number of place-based insights from local/indigenous communities representing important alternative worldviews.</p><p>The role of human influence in observed climate changes is evaluated using data from multiple gridded observational climate products and global climate models. We find that anthropogenic climate change has a clear and discernable fingerprint in changing natural and human mountain systems across the globe. In the cryosphere, ecosystems, water resources and tourism the contribution of anthropogenic climate change to observed changes is significant, showing the sensitivity of these systems to current and future climate change. Furthermore, our analysis reveals the need to consider the plurality of knowledge systems through which climate change impacts are being understood in mountain regions. Such attempts at inclusivity, which addresses issues of representation and justice, should be deemed necessary in exploring climate change impacts.</p>


2020 ◽  
Author(s):  
Christian Huggel ◽  
Mark Carey ◽  
Adam Emmer ◽  
Holger Frey ◽  
Noah Walker-Crawford ◽  
...  

Abstract. Evidence of observed negative impacts on natural and human systems from anthropogenic climate change is increasing. However, human systems in particular are dynamic and influenced by multiple drivers, and hence identifying an anthropogenic climate signal is challenging. Here we analyze the case of lake Palcacocha in the Andes of Peru which offers a representative model for other glacier lakes and related risks around the world because it features a dynamic evolution of flood risk driven by physical and socio-economic factors and processes. Furthermore, it is the object of a prominent climate litigation case where a local Peruvian citizen sued a large German energy producer over risk of flooding from lake Palcacocha. Adopting a conceptual model of cascading impacts and multiple drivers of risk we first study climatic and other geophysical drivers of flood risk. We find that an anthropogenic signal related to greenhouse gas emissions is traceable. In parallel, flood risk has been strongly shaped (and increased) by interacting socio-economic, institutional and cultural processes over the past decades. The case raises important questions of responsibility for flood risk of global and local agents which, however, are difficult to address in cases like Palcacocha where we reveal a complex network of interlinked global, national and local drivers. Following from this we outline a normative framework with a differentiated perspective on responsibility, implying that global emitters commit to support strengthening capacities in affected regions and localities, and local institutions and societies engage in local risk reduction measures and policies.


2020 ◽  
Vol 20 (8) ◽  
pp. 2175-2193 ◽  
Author(s):  
Christian Huggel ◽  
Mark Carey ◽  
Adam Emmer ◽  
Holger Frey ◽  
Noah Walker-Crawford ◽  
...  

Abstract. Evidence of observed negative impacts on natural and human systems from anthropogenic climate change is increasing. However, human systems in particular are dynamic and influenced by multiple drivers and hence identifying an anthropogenic climate signal is challenging. Here we analyze the case of lake Palcacocha in the Andes of Peru, which offers a representative model for other glacier lakes and related risks around the world because it features a dynamic evolution of flood risk driven by physical and socioeconomic factors and processes. Furthermore, it is the object of a prominent climate litigation case, wherein a local Peruvian citizen sued a large German energy producer over risk of flooding from lake Palcacocha. Adopting a conceptual model of cascading impacts and multiple drivers of risk, we first study climatic and other geophysical drivers of flood risk. We find that an anthropogenic signal from flood risk to greenhouse gas emissions is traceable. In parallel, flood risk has been strongly shaped (and increased) by interacting socioeconomic, institutional and cultural processes over the past few decades. The case raises important questions about the differentiation of responsibilities relating to flood risk of both global and local agents, which are, however, difficult to address in cases like Palcacocha, where we reveal a complex network of interlinked global, national and local drivers. Following from this, we outline a normative framework with a differentiated perspective on responsibility, implying that global emitters commit to support strengthening capacities in affected regions and localities and that local institutions and societies engage in local risk reduction measures and policies in collaboration with and driven by local communities.


2020 ◽  
Vol 12 (8) ◽  
pp. 3422 ◽  
Author(s):  
Paola A. Torres-Slimming ◽  
Carlee J. Wright ◽  
Guillermo Lancha ◽  
Cesar P. Carcamo ◽  
Patricia J. Garcia ◽  
...  

Climate change impacts on water systems have consequences for Indigenous communities. We documented climatic changes on water systems observed by Indigenous Shawi and resultant impacts on health and livelihoods, and explored adaptation options and challenges in partnership with two Indigenous Shawi communities in the Peruvian Amazon. Qualitative data were collected via PhotoVoice, interviews, focus group discussions, and transect walks, and analyzed using a constant comparative method and thematic analysis. Quantitative data were collected via a household survey and analyzed descriptively. Households observed seasonal weather changes over time (n = 50; 78%), which had already impacted their family and community (n = 43; 86%), such as more intense rainfall resulting in flooding (n = 29; 58%). Interviewees also described deforestation impacts on the nearby river, which were exacerbated by climate-related changes, including increased water temperatures (warmer weather, exacerbated by fewer trees for shading) and increased erosion and turbidity (increased rainfall, exacerbated by riverbank instability due to deforestation). No households reported community-level response plans for extreme weather events, and most did not expect government assistance when such events occurred. This study documents how Indigenous peoples are experiencing climatic impacts on water systems, and highlights how non-climatic drivers, such as deforestation, exacerbate climate change impacts on water systems and community livelihoods in the Peruvian Amazon.


2011 ◽  
Vol 17 (3) ◽  
pp. 220 ◽  
Author(s):  
Grant W Wardell-Johnson ◽  
Gunnar Keppel ◽  
Julianne Sander

We review the threats from anthropogenic climate change to the terrestrial biodiversity of Oceania, and quantify decline in carbon stocks. Oceania’s rich terrestrial biodiversity is facing unprecedented threats through the interaction of pervasive environmental threats (deforestation and degradation; introduced and invasive species; fragmentation) and the effects of anthropogenic climate change (sea level rise; altered rainfall patterns and increased fire frequency; temperature rises and increased storm severity, extreme weather events and abrupt system changes). All nine of Oceania’s terrestrial biomes harbour ecosystems and habitat types that are highly vulnerable under climate change, posing an immense conservation challenge. Current policies and management practices are inadequate and the need for new legislation and economic mechanisms is clear, despite powerful interests committed to limiting progress. Mitigation can be achieved by increasing the effectiveness of the protected area network, by maintaining and effectively managing existing carbon stocks and biodiversity, and by reforestation to sequester atmospheric carbon. A price on carbon emissions may encourage less carbon-intensive energy use while simultaneously encouraging reforestation on long-cleared land, and reducing degradation of native forests. However, realizing these changes will require societal change, and depend on input and collaboration from multiple stakeholders to devise and engage in shared, responsible management.


2021 ◽  
Vol 118 (7) ◽  
pp. e2013284118
Author(s):  
William R. L. Anderegg ◽  
John T. Abatzoglou ◽  
Leander D. L. Anderegg ◽  
Leonard Bielory ◽  
Patrick L. Kinney ◽  
...  

Airborne pollen has major respiratory health impacts and anthropogenic climate change may increase pollen concentrations and extend pollen seasons. While greenhouse and field studies indicate that pollen concentrations are correlated with temperature, a formal detection and attribution of the role of anthropogenic climate change in continental pollen seasons is urgently needed. Here, we use long-term pollen data from 60 North American stations from 1990 to 2018, spanning 821 site-years of data, and Earth system model simulations to quantify the role of human-caused climate change in continental patterns in pollen concentrations. We find widespread advances and lengthening of pollen seasons (+20 d) and increases in pollen concentrations (+21%) across North America, which are strongly coupled to observed warming. Human forcing of the climate system contributed ∼50% (interquartile range: 19–84%) of the trend in pollen seasons and ∼8% (4–14%) of the trend in pollen concentrations. Our results reveal that anthropogenic climate change has already exacerbated pollen seasons in the past three decades with attendant deleterious effects on respiratory health.


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