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A state-by-state look at how accelerating climate change is impacting or may impact fish and wildlife across America. The series provides a snapshot of the broad scope of changes and emerging trends we’re just beginning to understand, as well as collaborative efforts to respond across the nation.
Located in Resources / General Resources Holdings
The Conservation Challenge
Located in Cooperative / Our Plan / Section 1: Biodiversity and Conservation Challenges Across the Appalachian Region
File THE COST OF INACTION: RECOGNISING THE VALUE AT RISK FROM CLIMATE CHANGE
The asset management industry—and thus the wider community of investors of all sizes— is facing the prospect of significant losses from the effects of climate change. Assets can be directly damaged by floods, droughts and severe storms, but portfolios can also be harmed indirectly, through weaker growth and lower asset returns. Climate change is a long-term, probably irreversible problem beset by substantial uncertainty. Crucially, however, climate change is a problem of extreme risk: this means that the average losses to be expected are not the only source of concern; on the contrary, the outliers, the particularly extreme scenarios, may matter most of all.
Located in Resources / Climate Science Documents
The eDNA revolution & developing comprehensive aquatic biodiversity archives
Measuring & understanding the effects of climate change on aquatic life requires an accurate baseline status assessment that can serve as a benchmark for comparisons through time.
Located in News & Events
File The global volume and distribution of modern groundwater
Groundwater is important for energy and food security, human health and ecosystems. The time since groundwater was recharged—or groundwater age—can be important for diverse geologic processes, such as chemical weathering, ocean eutrophication and climate change. However, measured groundwater ages range from months to millions of years. The global volume and distribution of groundwater less than 50 years old—modern groundwater that is the most recently recharged and also the most vulnerable to global change—are unknown. Here we combine geochemical, geologic, hydrologic and geospatial data sets with numerical simulations of groundwater and analyse tritium ages to show that less than 6% of the groundwater in the uppermost portion of Earth’s landmass is modern. We find that the total groundwater volume in the upper 2 km of continental crust is approximately 22.6 million km3 , of which 0.1–5.0 million km3 is less than 50 years old. Although modern groundwater represents a small percentage of the total groundwater on Earth, the volume of modern groundwater is equivalent to a body of water with a depth of about 3 m spread over the continents. This water resource dwarfs all other components of the active hydrologic cycle.
Located in Resources / Climate Science Documents
File PDF document The Hot Summer of 2010: Redrawing the Temperature Record Map of Europe
The summer of 2010 was exceptionally warm in eastern Europe and large parts of Russia. We provide evidence that the anomalous 2010 warmth that caused adverse impacts exceeded the amplitude and spatial extent of the previous hottest summer of 2003. 'Mega-heatwaves' such as the 2003 and 2010 events broke the 500-yr long seasonal temperature records over approximately 50% of Europe. According to regional multi-model experiments, the probability of a summer experiencing 'megaheatwaves' will increase by a factor of 5 to 10 within the next 40 years. However, the magnitude of the 2010 event was so extreme that despite this increase, the occurrence of an analogue over the same region remains fairly unlikely until the second half of the 21st century.
Located in Resources / Climate Science Documents
File The links between ecosystem multifunctionality and above- and belowground biodiversity are mediated by climate
Plant biodiversity is often correlated with ecosystem functioning in terrestrial ecosystems. However, we know little about the relative and combined effects of above- and belowground biodiversity on multiple ecosystem functions (for example, ecosystem multifunctionality, EMF) or how climate might mediate those relationships. Here we tease apart the effects of biotic and abiotic factors, both above- and belowground, on EMF on the Tibetan Plateau, China. We found that a suite of biotic and abiotic variables account for up to 86% of the variation in EMF, with the combined effects of above- and belowground biodiversity accounting for 45% of the variation in EMF. Our results have two important implications: first, including belowground biodiversity in models can improve the ability to explain and predict EMF. Second, regional-scale variation in climate, and perhaps climate change, can determine, or at least modify, the effects of biodiversity on EMF in natural ecosystems.
Located in Resources / Climate Science Documents
The Nature Conservancy Releases Country-Level Temperature and Precipitation Data for Climate Resilience and Adaptation Planning
The Nature Conservancy has released a new country-level dataset for its online Climate Wizard mapping tool that enables users to visualize future climate conditions using the most recent modeled data from the Intergovernmental Panel on Climate Change (IPCC).
Located in News & Events
Climate Wizard enables technical and non-technical audiences alike to access leading climate change information and visualize the impacts anywhere on Earth. The first generation of this web-based program allows the user to choose a state or country and both assess how climate has changed over time and to project what future changes are predicted to occur in a given area.
Located in Planning In Practice / Conservation Planning Projects
The Planning for Growth and Open Space Conservation Webinar Series
Planning for Climate Change Adaptation: Considerations for Forests, Wildlife, and Land Use
Located in News & Events / Events