uri,href,identifier,attrs.Abstract,attrs.Author,attrs.DOI,attrs.Issue,attrs.Journal,attrs.Keywords,attrs.Pages,attrs.Title,attrs.Volume,attrs.Year,attrs._record_number,attrs._uuid,attrs.reftype,child_publication
/reference/da714e9f-808c-4aae-8d24-aef041988322,https://data.globalchange.gov/reference/da714e9f-808c-4aae-8d24-aef041988322,da714e9f-808c-4aae-8d24-aef041988322,"In recent years increasing attention has been focused on understanding the different resources that can support decision makers at all levels in responding to climate variability and change. This article focuses on the role that access to information and other potential constraints may play in the context of water decision making across three U.S. regions (the Intermountain West, the Great Lakes, and the Carolinas). The authors report on the degree to which climate-related needs or constraints pertinent to water resources are regionally specific. They also find that stakeholder-identified constraints or needs extended beyond the need for data/information to enabling factors such as governance arrangements and how to improve collaboration and communication. As climate information networks expand and emphasis is placed on encouraging adaptation more broadly, these constraints have implications not only for how information dissemination efforts are organized but for how those efforts need to be informed by the larger regional context in a resource-limited and fragmented landscape.","Dilling, Lisa; Kirsten Lackstrom; Benjamin Haywood; Kirstin Dow; Maria Carmen Lemos; John Berggren; Scott Kalafatis",10.1175/wcas-d-14-00001.1,1,"Weather, Climate, and Society","Climate change,Climate variability,Policy,Societal impacts",5-17,"What stakeholder needs tell us about enabling adaptive capacity: The intersection of context and information provision across regions in the United States",7,2015,26359,da714e9f-808c-4aae-8d24-aef041988322,"Journal Article",/article/10.1175/wcas-d-14-00001.1
/reference/da90ef66-3e0e-4b0c-a7ea-c0503b993cb2,https://data.globalchange.gov/reference/da90ef66-3e0e-4b0c-a7ea-c0503b993cb2,da90ef66-3e0e-4b0c-a7ea-c0503b993cb2,,"Bucci, Monica; Marques, Sara Silvério; Oh, Debora; Harris, Nadine Burke",10.1016/j.yapd.2016.04.002,1,"Advances in Pediatrics",,403-428,"Toxic stress in children and adolescents",63,2016,23734,da90ef66-3e0e-4b0c-a7ea-c0503b993cb2,"Journal Article",/article/10.1016/j.yapd.2016.04.002
/reference/dca58e36-d2c9-43af-b3fd-67338f710de9,https://data.globalchange.gov/reference/dca58e36-d2c9-43af-b3fd-67338f710de9,dca58e36-d2c9-43af-b3fd-67338f710de9,"California's primary hydrologic system, the San Francisco estuary and its upstream watershed, is vulnerable to the regional hydrologic consequences of projected global climate change. Projected temperature anomalies from a global climate model are used to drive a combined model of watershed hydrology and estuarine dynamics. By 2090, a projected temperature increase of 2.1°C results in a loss of about half of the average April snowpack storage, with greatest losses in the northern headwaters. Consequently, spring runoff is reduced by 5.6 km3 (∼20% of historical annual runoff), with associated increases in winter flood peaks. The smaller spring flows yield spring/summer salinity increases of up to 9 psu, with larger increases in wet years.","Knowles, Noah; Cayan, Daniel R.",10.1029/2001GL014339,18,"Geophysical Research Letters",,1891,"Potential effects of global warming on the Sacramento/San Joaquin watershed and the San Francisco estuary",29,2002,26371,dca58e36-d2c9-43af-b3fd-67338f710de9,"Journal Article",/article/10.1029/2001GL014339
/reference/dd11662f-f1a1-4a3b-a34f-295e5364e5ed,https://data.globalchange.gov/reference/dd11662f-f1a1-4a3b-a34f-295e5364e5ed,dd11662f-f1a1-4a3b-a34f-295e5364e5ed,,"Henson, Stephanie A.; Beaulieu, Claudie; Ilyina, Tatiana; John, Jasmin G.; Long, Matthew; Séférian, Roland; Tjiputra, Jerry; Sarmiento, Jorge L.",10.1038/ncomms14682,,"Nature Communications",,14682,"Rapid emergence of climate change in environmental drivers of marine ecosystems",8,2017,22449,dd11662f-f1a1-4a3b-a34f-295e5364e5ed,"Journal Article",/article/10.1038/ncomms14682
/reference/dd9585ac-dc38-4e88-9899-edebb82d51f6,https://data.globalchange.gov/reference/dd9585ac-dc38-4e88-9899-edebb82d51f6,dd9585ac-dc38-4e88-9899-edebb82d51f6,,"Crouch, Jake; Heim, Richard R.; Hughes, P. E.; Fenimore, Chris",10.1175/2013BAMSStateoftheClimate.1,8,"Bulletin of the American Meteorological Society",,S149-S152,"Regional climates: United States [in ""State of the Climate in 2012""]",94,2013,26354,dd9585ac-dc38-4e88-9899-edebb82d51f6,"Journal Article",/article/10.1175/2013BAMSStateoftheClimate.1
/reference/dde395ae-d68c-4fdd-b3c8-d1ccbee85102,https://data.globalchange.gov/reference/dde395ae-d68c-4fdd-b3c8-d1ccbee85102,dde395ae-d68c-4fdd-b3c8-d1ccbee85102,,"Slangen, Aimee B. A.; Church, John A.; Agosta, Cecile; Fettweis, Xavier; Marzeion, Ben; Richter, Kristin",10.1038/nclimate2991,,"Nature Climate Change",,701-705,"Anthropogenic forcing dominates global mean sea-level rise since 1970",6,2016,19982,dde395ae-d68c-4fdd-b3c8-d1ccbee85102,"Journal Article",/article/10.1038/nclimate2991
/reference/de4a77df-03ba-4319-a13f-7fdefbb353a5,https://data.globalchange.gov/reference/de4a77df-03ba-4319-a13f-7fdefbb353a5,de4a77df-03ba-4319-a13f-7fdefbb353a5,"Increased forest fire activity across the western continental United States (US) in recent decades has likely been enabled by a number of factors, including the legacy of fire suppression and human settlement, natural climate variability, and human-caused climate change. We use modeled climate projections to estimate the contribution of anthropogenic climate change to observed increases in eight fuel aridity metrics and forest fire area across the western United States. Anthropogenic increases in temperature and vapor pressure deficit significantly enhanced fuel aridity across western US forests over the past several decades and, during 2000–2015, contributed to 75% more forested area experiencing high (>1 σ) fire-season fuel aridity and an average of nine additional days per year of high fire potential. Anthropogenic climate change accounted for ∼55% of observed increases in fuel aridity from 1979 to 2015 across western US forests, highlighting both anthropogenic climate change and natural climate variability as important contributors to increased wildfire potential in recent decades. We estimate that human-caused climate change contributed to an additional 4.2 million ha of forest fire area during 1984–2015, nearly doubling the forest fire area expected in its absence. Natural climate variability will continue to alternate between modulating and compounding anthropogenic increases in fuel aridity, but anthropogenic climate change has emerged as a driver of increased forest fire activity and should continue to do so while fuels are not limiting.","Abatzoglou, John T.; Williams, A. Park",10.1073/pnas.1607171113,42,"Proceedings of the National Academy of Sciences of the United States of America",,11770-11775,"Impact of anthropogenic climate change on wildfire across western US forests",113,2016,20416,de4a77df-03ba-4319-a13f-7fdefbb353a5,"Journal Article",/article/10.1073/pnas.1607171113
/reference/debdf209-4050-4706-965c-09cff7ec353b,https://data.globalchange.gov/reference/debdf209-4050-4706-965c-09cff7ec353b,debdf209-4050-4706-965c-09cff7ec353b,,"Voggesser, Garrit
Lynn, Kathy
Daigle, John
Lake, Frank K.
Ranco, Darren",10.1007/s10584-013-0733-4,3,"Climatic Change",,615-626,"Cultural impacts to tribes from climate change influences on forests",120,2013,3852,debdf209-4050-4706-965c-09cff7ec353b,"Journal Article",/article/10.1007/s10584-013-0733-4
/reference/df25e033-b388-4aab-b7a4-00d6a9ef3e7e,https://data.globalchange.gov/reference/df25e033-b388-4aab-b7a4-00d6a9ef3e7e,df25e033-b388-4aab-b7a4-00d6a9ef3e7e,,"Klos, P. Zion; Link, Timothy E.; Abatzoglou, John T.",10.1002/2014GL060500,13,"Geophysical Research Letters","precipitation phase; rain-snow transition; rain snow transition; climate change; 0736 Snow; 1621 Cryospheric change; 1637 Regional climate change; 1854 Precipitation; 1840 Hydrometeorology",4560-4568,"Extent of the rain–snow transition zone in the western U.S. under historic and projected climate",41,2014,20539,df25e033-b388-4aab-b7a4-00d6a9ef3e7e,"Journal Article",/article/10.1002/2014GL060500
/reference/e02079e4-6160-4552-8493-ba80eeeeff8c,https://data.globalchange.gov/reference/e02079e4-6160-4552-8493-ba80eeeeff8c,e02079e4-6160-4552-8493-ba80eeeeff8c,,"Sherson, Lauren R.; Van Horn, David J.; Gomez-Velez, Jesus D.; Crossey, Laura J.; Dahm, Clifford N.",10.1002/hyp.10426,14,"Hydrological Processes","nutrient dynamics; continuous monitoring; wildfire; monsoonal storms; water quality; headwater streams",3193-3207,"Nutrient dynamics in an alpine headwater stream: Use of continuous water quality sensors to examine responses to wildfire and precipitation events",29,2015,23855,e02079e4-6160-4552-8493-ba80eeeeff8c,"Journal Article",/article/10.1002/hyp.10426
/reference/e028e561-0d0d-4ebd-acc0-5aa92fc73750,https://data.globalchange.gov/reference/e028e561-0d0d-4ebd-acc0-5aa92fc73750,e028e561-0d0d-4ebd-acc0-5aa92fc73750,,"Stewart, Joseph A. E.; Perrine, John D.; Nichols, Lyle B.; Thorne, James H.; Millar, Constance I.; Goehring, Kenneth E.; Massing, Cody P.; Wright, David H.",10.1111/jbi.12466,5,"Journal of Biogeography","Climate change; global warming; historical resurvey; metapopulation; Ochotona princeps; pika; range shift; species distribution modelling; talus",880-890,"Revisiting the past to foretell the future: Summer temperature and habitat area predict pika extirpations in California",42,2015,23865,e028e561-0d0d-4ebd-acc0-5aa92fc73750,"Journal Article",/article/10.1111/jbi.12466
/reference/e0d237d0-bc2d-4538-9eb0-4732237cae82,https://data.globalchange.gov/reference/e0d237d0-bc2d-4538-9eb0-4732237cae82,e0d237d0-bc2d-4538-9eb0-4732237cae82,,"Writer, Jeffrey H.; Hohner, Amanda; Oropeza, Jill; Schmidt, Amanda; Cawley, Kaelin M.; Rosario-Ortiz, Fernando L.",10.5942/jawwa.2014.106.0055,4,"Journal—American Water Works Association",,E189-E199,"Water treatment implications after the High Park Wildfire, Colorado",106,2014,23889,e0d237d0-bc2d-4538-9eb0-4732237cae82,"Journal Article",/article/10.5942/jawwa.2014.106.0055
/reference/e126059c-67f3-4522-8381-ae2499296312,https://data.globalchange.gov/reference/e126059c-67f3-4522-8381-ae2499296312,e126059c-67f3-4522-8381-ae2499296312,"The 2012–2015 drought has left California with severely reduced snowpack, soil moisture, ground water, and reservoir stocks, but the impact of this estimated millennial-scale event on forest health is unknown. We used airborne laser-guided spectroscopy and satellite-based models to assess losses in canopy water content of California’s forests between 2011 and 2015. Approximately 10.6 million ha of forest containing up to 888 million large trees experienced measurable loss in canopy water content during this drought period. Severe canopy water losses of greater than 30% occurred over 1 million ha, affecting up to 58 million large trees. Our measurements exclude forests affected by fire between 2011 and 2015. If drought conditions continue or reoccur, even with temporary reprieves such as El Niño, we predict substantial future forest change.","Asner, Gregory P.; Brodrick, Philip G.; Anderson, Christopher B.; Vaughn, Nicholas; Knapp, David E.; Martin, Roberta E.",10.1073/pnas.1523397113,2,"Proceedings of the National Academy of Sciences of the United States of America",,E249-E255,"Progressive forest canopy water loss during the 2012–2015 California drought",113,2016,19775,e126059c-67f3-4522-8381-ae2499296312,"Journal Article",/article/10.1073/pnas.1523397113
/reference/e1dd379b-04d7-447d-ac40-27ed82995e4c,https://data.globalchange.gov/reference/e1dd379b-04d7-447d-ac40-27ed82995e4c,e1dd379b-04d7-447d-ac40-27ed82995e4c,,"Largier, John; Brian Cheng; Kelley Higgason",,,,,121,"Climate Change Impacts: Gulf of the Farallones and Cordell Bank National Marine Sanctuaries",,2011,23938,e1dd379b-04d7-447d-ac40-27ed82995e4c,Report,/report/climate-change-impacts-gulf-farallones-cordell-bank-national-marine-sanctuaries
/reference/e22493ce-7924-4036-90f4-9c0e69ddfcfd,https://data.globalchange.gov/reference/e22493ce-7924-4036-90f4-9c0e69ddfcfd,e22493ce-7924-4036-90f4-9c0e69ddfcfd,,"Tarroja, Brian; AghaKouchak, Amir; Samuelsen, Scott",10.1016/j.energy.2016.05.131,,Energy,"Hydropower; Hydroelectricity; Climate change; Greenhouse gas emissions; Electric grid",295-305,"Quantifying climate change impacts on hydropower generation and implications on electric grid greenhouse gas emissions and operation",111,2016,23869,e22493ce-7924-4036-90f4-9c0e69ddfcfd,"Journal Article",/article/10.1016/j.energy.2016.05.131
/reference/e251f590-177e-4ba6-8ed1-6f68b5e54c8a,https://data.globalchange.gov/reference/e251f590-177e-4ba6-8ed1-6f68b5e54c8a,e251f590-177e-4ba6-8ed1-6f68b5e54c8a,,,,,,,,"Global Climate Change Impacts in the United States",,2009,769,e251f590-177e-4ba6-8ed1-6f68b5e54c8a,"Edited Book",/report/nca2
/reference/e2ad8754-f271-4960-b198-51edd21e2e04,https://data.globalchange.gov/reference/e2ad8754-f271-4960-b198-51edd21e2e04,e2ad8754-f271-4960-b198-51edd21e2e04,,"Munson, Seth M.; Webb, Robert H.; Belnap, Jayne; Hubbard, J.A.; Swann, Don E.; Rutman, Sue",10.1111/j.1365-2486.2011.02598.x,3,"Global Change Biology","arid; drought; long-term change; plant cover; southwestern United States",1083-1095,"Forecasting climate change impacts to plant community composition in the Sonoran Desert region",18,2012,14640,e2ad8754-f271-4960-b198-51edd21e2e04,"Journal Article",/article/10.1111/j.1365-2486.2011.02598.x
/reference/e2cbf775-6f83-4a51-8042-010716f7d47e,https://data.globalchange.gov/reference/e2cbf775-6f83-4a51-8042-010716f7d47e,e2cbf775-6f83-4a51-8042-010716f7d47e,"Climate change is likely to affect the generation of energy from California’s high-elevation hydropower systems. To investigate these impacts, this study formulates a linear programming model of an 11-reservoir hydroelectric system operated by the Sacramento Municipal Utility District in the Upper American River basin. Four sets of hydrologic scenarios are developed using the Variable Infiltration Capacity model combined with climatic output from two general circulation models under two greenhouse-gas emissions scenarios. Power generation and revenues fall under two of the four climate change scenarios, as a consequence of drier hydrologic conditions. Energy generation is primarily limited by annual volume of streamflow, and is affected more than revenues, reflecting the ability of the system to store water when energy prices are low for use when prices are high (July through September). Power generation and revenues increase for two of the scenarios, which predict wetter hydrologic conditions. In this case, power generation increases more than revenues indicating that the system is using most of its available capacity under current hydrologic conditions. Hydroelectric systems located in basins with hydrograph centroids occuring close to summer months (July through September) are likely to be affected by the changes in hydrologic timing associated with climate change (e.g., earlier snowmelts and streamflows) if the systems lack sufficient storage capacity. High Sierra hydroelectric systems with sufficiently large storage capacity should not be affected by climate-induced changes in hydrologic timing.","Vicuna, S.; Leonardson, R.; Hanemann, M. W.; Dale, L. L.; Dracup, J. A.",10.1007/s10584-007-9365-x,1,"Climatic Change",,123-137,"Climate change impacts on high elevation hydropower generation in California’s Sierra Nevada: A case study in the Upper American River",87,2008,26397,e2cbf775-6f83-4a51-8042-010716f7d47e,"Journal Article",/article/10.1007/s10584-007-9365-x
/reference/e353701d-b2bf-4ddd-af78-6bced072e963,https://data.globalchange.gov/reference/e353701d-b2bf-4ddd-af78-6bced072e963,e353701d-b2bf-4ddd-af78-6bced072e963,,"Millar, C. I.
Westfall, R. D.
Delany, D. L.
King, J. C.
Graumlich, L. J.",10.1657/1523-0430(2004)036[0181:roscit]2.0.co;2,2,"Arctic, Antarctic, and Alpine Research",,181-200,"Response of subalpine conifers in the Sierra Nevada, California, USA, to 20th-century warming and decadal climate variability",36,2004,2029,e353701d-b2bf-4ddd-af78-6bced072e963,"Journal Article",/article/10.1657/1523-0430(2004)036%5B0181:roscit%5D2.0.co;2
/reference/e450ba2c-db69-43c8-8af4-e0c8ce7c8f2f,https://data.globalchange.gov/reference/e450ba2c-db69-43c8-8af4-e0c8ce7c8f2f,e450ba2c-db69-43c8-8af4-e0c8ce7c8f2f,"Mountain snowpack stores a significant quantity of water in the western US, accumulating during the wet season and melting during the dry summers and supplying much of the water used for irrigated agriculture, and municipal and industrial uses. Updating our earlier work published in 2005, we find that with 14 additional years of data, over 90% of snow monitoring sites with long records across the western US now show declines, of which 33% are significant (vs. 5% expected by chance) and 2% are significant and positive (vs. 5% expected by chance). Declining trends are observed across all months, states, and climates, but are largest in spring, in the Pacific states, and in locations with mild winter climate. We corroborate and extend these observations using a gridded hydrology model, which also allows a robust estimate of total western snowpack and its decline. We find a large increase in the fraction of locations that posted decreasing trends, and averaged across the western US, the decline in average April 1 snow water equivalent since mid-century is roughly 15–30% or 25–50 km3, comparable in volume to the West’s largest man-made reservoir, Lake Mead.","Mote, Philip W.; Li, Sihan; Lettenmaier, Dennis P.; Xiao, Mu; Engel, Ruth",10.1038/s41612-018-0012-1,1,"npj Climate and Atmospheric Science",,2,"Dramatic declines in snowpack in the western US",1,2018,25165,e450ba2c-db69-43c8-8af4-e0c8ce7c8f2f,"Journal Article",/article/10.1038/s41612-018-0012-1
/reference/e4a5a03e-0138-4ebb-98ad-6fb28ec56be5,https://data.globalchange.gov/reference/e4a5a03e-0138-4ebb-98ad-6fb28ec56be5,e4a5a03e-0138-4ebb-98ad-6fb28ec56be5,"The highly variable timing of streamflow in snowmelt-dominated basins across western North America is an important consequence, and indicator, of climate fluctuations. Changes in the timing of snowmelt-derived streamflow from 1948 to 2002 were investigated in a network of 302 western North America gauges by examining the center of mass for flow, spring pulse onset dates, and seasonal fractional flows through trend and principal component analyses. Statistical analysis of the streamflow timing measures with Pacific climate indicators identified local and key large-scale processes that govern the regionally coherent parts of the changes and their relative importance.|Widespread and regionally coherent trends toward earlier onsets of springtime snowmelt and streamflow have taken place across most of western North America, affecting an area that is much larger than previously recognized. These timing changes have resulted in increasing fractions of annual flow occurring earlier in the water year by 1-4 weeks. The immediate (or proximal) forcings for the spatially coherent parts of the year-to-year fluctuations and longer-term trends of streamflow timing have been higher winter and spring temperatures. Although these temperature changes are partly controlled by the decadal-scale Pacific climate mode [Pacific decadal oscillation (PDO)], a separate ani significant part of the variance is associated with a springtime warming trend that spans the PDO phases.","Stewart, I.T.
Cayan, D.R.
Dettinger, M.D.",10.1175/JCLI3321.1,8,"Journal of Climate","UNITED-STATES; CLIMATE-CHANGE; MASS-BALANCE; ATMOSPHERIC CIRCULATION; PACIFIC-NORTHWEST; SNOWMELT RUNOFF; SIERRA-NEVADA; RIVER-BASIN; VARIABILITY; PRECIPITATION",1136-1155,"Changes toward earlier streamflow timing across western North America",18,2005,2957,e4a5a03e-0138-4ebb-98ad-6fb28ec56be5,"Journal Article",/article/10.1175/JCLI3321.1
/reference/e4c07020-0c97-4a6c-ab4a-1859aaebd5ab,https://data.globalchange.gov/reference/e4c07020-0c97-4a6c-ab4a-1859aaebd5ab,e4c07020-0c97-4a6c-ab4a-1859aaebd5ab,,"Luber, George
McGeehin, Michael",10.1016/j.amepre.2008.08.021,5,"American Journal of Preventive Medicine",,429-435,"Climate change and extreme heat events",35,2008,4293,e4c07020-0c97-4a6c-ab4a-1859aaebd5ab,"Journal Article",/article/10.1016/j.amepre.2008.08.021
/reference/e523f9c0-56f9-44ff-b2d9-7debec2a19d0,https://data.globalchange.gov/reference/e523f9c0-56f9-44ff-b2d9-7debec2a19d0,e523f9c0-56f9-44ff-b2d9-7debec2a19d0,,"Hirshon, Jon Mark; Alson, Roy L.; Blunk, David; Brosnan, Douglas P.; Epstein, Stephen K.; Gardner, Angela F.; Lum, Donald L.; Moskovitz, Joshua B.; Richardson, Lynne D.; Stankus, Jennifer L.; Kivela, Paul D.; Wilkerson, Dean; Price, Craig; Bromley, Marilyn; Calaway, Nancy; Geist, Marjorie; Gore, Laura; Singh, Cynthia; Wheeler, Gordon",10.1016/j.annemergmed.2013.11.024,2,"Annals of Emergency Medicine",,100-243,"America's emergency care environment, a state-by-state report card",63,2014,23847,e523f9c0-56f9-44ff-b2d9-7debec2a19d0,"Journal Article",/article/10.1016/j.annemergmed.2013.11.024
/reference/e56d8268-7bc7-4d40-a36f-21bfbf54a7cf,https://data.globalchange.gov/reference/e56d8268-7bc7-4d40-a36f-21bfbf54a7cf,e56d8268-7bc7-4d40-a36f-21bfbf54a7cf,"Climate projections for the southwestern US suggest a warmer, drier future and have the potential to impact forest carbon (C) sequestration and post-fire C recovery. Restoring forest structure and surface fire regimes initially decreases total ecosystem carbon (TEC), but can stabilize the remaining C by moderating wildfire behavior. Previous research has demonstrated that fire maintained forests can store more C over time than fire suppressed forests in the presence of wildfire. However, because the climate future is uncertain, I sought to determine the efficacy of forest management to moderate fire behavior and its effect on forest C dynamics under current and projected climate. I used the LANDIS-II model to simulate carbon dynamics under early (2010–2019), mid (2050–2059), and late (2090–2099) century climate projections for a ponderosa pine (Pinus ponderosa) dominated landscape in northern Arizona. I ran 100-year simulations with two different treatments (control, thin and burn) and a 1 in 50 chance of wildfire occurring. I found that control TEC had a consistent decline throughout the simulation period, regardless of climate. Thin and burn TEC increased following treatment implementation and showed more differentiation than the control in response to climate, with late-century climate having the lowest TEC. Treatment efficacy, as measured by mean fire severity, was not impacted by climate. Fire effects were evident in the cumulative net ecosystem exchange (NEE) for the different treatments. Over the simulation period, 32.8–48.9% of the control landscape was either C neutral or a C source to the atmosphere and greater than 90% of the thin and burn landscape was a moderate C sink. These results suggest that in southwestern ponderosa pine, restoring forest structure and surface fire regimes provides a reasonable hedge against the uncertainty of future climate change for maintaining the forest C sink.","Hurteau, Matthew D.",10.1371/journal.pone.0169275,1,"PLOS ONE",,e0169275,"Quantifying the carbon balance of forest restoration and wildfire under projected climate in the fire-prone southwestern US",12,2017,23678,e56d8268-7bc7-4d40-a36f-21bfbf54a7cf,"Journal Article",/article/10.1371/journal.pone.0169275
/reference/e6404db9-fef8-42ba-95c8-3a7c5b7d8d05,https://data.globalchange.gov/reference/e6404db9-fef8-42ba-95c8-3a7c5b7d8d05,e6404db9-fef8-42ba-95c8-3a7c5b7d8d05,,"Mawdsley, Jonathan; Lamb, Rachel",,,,,49,"Climate change vulnerability assessment for priority wildlife species",,2013,26377,e6404db9-fef8-42ba-95c8-3a7c5b7d8d05,Report,/report/climate-change-vulnerability-assessment-priority-wildlife-species