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      Large Reductions in Temperate Rainforest Biome Due to Unmitigated Climate Change

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          Abstract

          Temperate rainforests are rare ecosystems globally; restricted to cool, moist conditions that are sensitive to a changing climate. Despite their crucial conservation importance, a global assessment of how temperate rainforests will be impacted by climate change is lacking. We calculated historical (1970–2000) climate conditions for the temperate rainforest biome using ERA5 reanalysis data for three key bioclimatic variables: warmest quarter temperature, annual precipitation and proportion of rainfall during warmest quarter. We used high‐spatial resolution climate projections for these variables to identify regions likely to become unsuitable for temperate rainforests under four future shared socioeconomic pathway (SSP) scenarios. We predict unmitigated climate change (SSP 5–8.5) would lead to a 68.3 (95% confidence interval (95 CI): 53.4–81.3)% loss in the existing temperate rainforest biome by 2100 at a global scale with some national‐level reductions exceeding 90%. Restricting global warming to <2°C (consistent with SSP 1–2.6), limits loss of global temperate rainforest biome to 9.7 (95 CI: 7.8–13.3)% by 2100 and is crucial to ensuring temperate rainforest persistence. Deforestation has resulted in loss of up to 43% of the current temperate rainforest biome with only 37% of primary forest remaining, and some regions like Europe with virtually none. Protection and restoration of the temperate rainforest biome, along with emissions reductions, are vital to its climate future.

          Plain Language Summary

          Temperate rainforests are rare ecosystems found only in wet and cool regions, making them vulnerable to a warming climate. They are important to conserve because they host unique species and can store high amounts of carbon. We use global maps of forest cover and condition to assess how much temperate rainforest remains, and how much it has been impacted by human activity. We find that only 37% of the temperate rainforest area is still covered by primary forest. We use a map of existing temperate rainforests along with records of past weather conditions to estimate what climate conditions are needed for its survival. We then use estimates of future climate under four different scenarios of greenhouse gas emissions to see which areas of temperate rainforest will maintain these conditions up to 2100. We find that under the most pessimistic scenario, 68% of temperate rainforest will be lost, while under the most optimistic scenario, only 9% will be lost. Our study can aid temperate rainforest conservation by identifying the areas of temperate rainforest that are least/most vulnerable to climate change, and where there is potential to restore forest.

          Key Points

          • Temperate rainforests rely on a cool and moist climate biome that globally rare and vulnerable to climate change

          • Unmitigated climate change would lead to a loss of 68% of the temperate rainforest biome, but climate mitigation limits loss to 9%

          • We identify historical, intact and potential temperate rainforest extent and climate change vulnerability to inform conservation efforts

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          Most cited references49

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          WorldClim 2: new 1-km spatial resolution climate surfaces for global land areas

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            The ERA5 Global Reanalysis

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              Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization

              By coordinating the design and distribution of global climate model simulations of the past, current, and future climate, the Coupled Model Intercomparison Project (CMIP) has become one of the foundational elements of climate science. However, the need to address an ever-expanding range of scientific questions arising from more and more research communities has made it necessary to revise the organization of CMIP. After a long and wide community consultation, a new and more federated structure has been put in place. It consists of three major elements: (1) a handful of common experiments, the DECK (Diagnostic, Evaluation and Characterization of Klima) and CMIP historical simulations (1850–near present) that will maintain continuity and help document basic characteristics of models across different phases of CMIP; (2) common standards, coordination, infrastructure, and documentation that will facilitate the distribution of model outputs and the characterization of the model ensemble; and (3) an ensemble of CMIP-Endorsed Model Intercomparison Projects (MIPs) that will be specific to a particular phase of CMIP (now CMIP6) and that will build on the DECK and CMIP historical simulations to address a large range of specific questions and fill the scientific gaps of the previous CMIP phases. The DECK and CMIP historical simulations, together with the use of CMIP data standards, will be the entry cards for models participating in CMIP. Participation in CMIP6-Endorsed MIPs by individual modelling groups will be at their own discretion and will depend on their scientific interests and priorities. With the Grand Science Challenges of the World Climate Research Programme (WCRP) as its scientific backdrop, CMIP6 will address three broad questions: – How does the Earth system respond to forcing? – What are the origins and consequences of systematic model biases? – How can we assess future climate changes given internal climate variability, predictability, and uncertainties in scenarios? This CMIP6 overview paper presents the background and rationale for the new structure of CMIP, provides a detailed description of the DECK and CMIP6 historical simulations, and includes a brief introduction to the 21 CMIP6-Endorsed MIPs.
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                Author and article information

                Contributors
                Journal
                Earth's Future
                Earth's Future
                American Geophysical Union (AGU)
                2328-4277
                2328-4277
                November 2024
                November 12 2024
                November 2024
                : 12
                : 11
                Affiliations
                [1 ] School of Earth and Environment University of Leeds Leeds UK
                [2 ] Wild Heritage, a Project of Earth Island Institute Berkeley CA USA
                Article
                10.1029/2024EF004812
                ad2844d8-9a9c-4c40-a774-6d7e5bbf17bc
                © 2024

                http://creativecommons.org/licenses/by/4.0/

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