uri,href,identifier,attrs.Abstract,attrs.Author,attrs.DOI,attrs.Date,attrs.Issue,attrs.Journal,attrs.Pages,attrs.Title,attrs.Volume,attrs.Year,attrs.\.reference_type,attrs._record_number,attrs._uuid,attrs.reftype,child_publication
/reference/89e08a41-6091-45fa-a92e-6168a90a8151,https://data.globalchange.gov/reference/89e08a41-6091-45fa-a92e-6168a90a8151,89e08a41-6091-45fa-a92e-6168a90a8151,"California is currently in the midst of a record-setting drought. The drought began in 2012 and now includes the lowest calendar-year and 12-mo precipitation, the highest annual temperature, and the most extreme drought indicators on record. The extremely warm and dry conditions have led to acute water shortages, groundwater overdraft, critically low streamflow, and enhanced wildfire risk. Analyzing historical climate observations from California, we find that precipitation deficits in California were more than twice as likely to yield drought years if they occurred when conditions were warm. We find that although there has not been a substantial change in the probability of either negative or moderately negative precipitation anomalies in recent decades, the occurrence of drought years has been greater in the past two decades than in the preceding century. In addition, the probability that precipitation deficits co-occur with warm conditions and the probability that precipitation deficits produce drought have both increased. Climate model experiments with and without anthropogenic forcings reveal that human activities have increased the probability that dry precipitation years are also warm. Further, a large ensemble of climate model realizations reveals that additional global warming over the next few decades is very likely to create ∼100% probability that any annual-scale dry period is also extremely warm. We therefore conclude that anthropogenic warming is increasing the probability of co-occurring warm–dry conditions like those that have created the acute human and ecosystem impacts associated with the “exceptional” 2012–2014 drought in California.","Diffenbaugh, Noah S.; Swain, Daniel L.; Touma, Danielle",10.1073/pnas.1422385112,"March 31, 2015",13,"Proceedings of the National Academy of Sciences of the United States of America",3931-3936,"Anthropogenic warming has increased drought risk in California",112,2015,0,19545,89e08a41-6091-45fa-a92e-6168a90a8151,"Journal Article",/article/10.1073/pnas.1422385112
/reference/8a61b1a7-bb52-496d-86f7-21911efcf5f8,https://data.globalchange.gov/reference/8a61b1a7-bb52-496d-86f7-21911efcf5f8,8a61b1a7-bb52-496d-86f7-21911efcf5f8,"Adaptation planning offers a promising approach for identifying and devising solutions to address local climate change impacts. Yet there is little empirical understanding of the content and quality of these plans. We use content analysis to evaluate 44 local adaptation plans in the United States and multivariate regression to examine how plan quality varies across communities. We find that plans draw on multiple data sources to analyse future climate impacts and include a breadth of strategies. Most plans, however, fail to prioritize impacts and strategies or provide detailed implementation processes, raising concerns about whether adaptation plans will translate into on-the-ground reductions in vulnerability. Our analysis also finds that plans authored by the planning department and those that engaged elected officials in the planning process were of higher quality. The results provide important insights for practitioners, policymakers and scientists wanting to improve local climate adaptation planning and action.","Woodruff, Sierra C.; Stults, Missy",10.1038/nclimate3012,08//print,8,"Nature Climate Change",796-802,"Numerous strategies but limited implementation guidance in US local adaptation plans",6,2016,,21160,8a61b1a7-bb52-496d-86f7-21911efcf5f8,"Journal Article",/article/10.1038/nclimate3012
/reference/8acf6392-b55f-4fbe-a660-1777e06b6607,https://data.globalchange.gov/reference/8acf6392-b55f-4fbe-a660-1777e06b6607,8acf6392-b55f-4fbe-a660-1777e06b6607,"Temperature and airport elevation significantly influence the maximum allowable takeoff weight of an aircraft by changing the surface air density and thus the lift produced at a given speed. For a given runway length, airport elevation, and aircraft type, there is a temperature threshold above which the airplane cannot take off at its maximum weight and thus must be weight restricted. The number of summer days necessitating weight restriction has increased since 1980 along with the observed increase in surface temperature. Climate change is projected to increase mean temperatures at all airports and to significantly increase the frequency and severity of extreme heat events at some. These changes will negatively affect aircraft performance, leading to increased weight restrictions, especially at airports with short runways and little room to expand. For a Boeing 737-800 aircraft, it was found that the number of weight-restriction days between May and September will increase by 50%–200% at four major airports in the United States by 2050–70 under the RCP8.5 emissions scenario. These performance reductions may have a negative economic effect on the airline industry. Increased weight restrictions have previously been identified as potential impacts of climate change, but this study is the first to quantify the effect of higher temperatures on commercial aviation. Planning for changes in extreme heat events will help the aviation industry to reduce its vulnerability to this aspect of climate change.","Coffel, E.; R. Horton",10.1175/wcas-d-14-00026.1,,1,"Weather, Climate, and Society",94-102,"Climate change and the impact of extreme temperatures on aviation",7,2015,,24541,8acf6392-b55f-4fbe-a660-1777e06b6607,"Journal Article",/article/10.1175/wcas-d-14-00026.1
/reference/8c12cc4c-3448-4055-b7a2-e03ead1c2572,https://data.globalchange.gov/reference/8c12cc4c-3448-4055-b7a2-e03ead1c2572,8c12cc4c-3448-4055-b7a2-e03ead1c2572,,"van Vliet, Michelle T. H.; Wiberg, David; Leduc, Sylvain; Riahi, Keywan",10.1038/nclimate2903,04//print,4,"Nature Climate Change",375-380,"Power-generation system vulnerability and adaptation to changes in climate and water resources",6,2016,,21334,8c12cc4c-3448-4055-b7a2-e03ead1c2572,"Journal Article",/article/10.1038/nclimate2903
/reference/8c622c97-0a72-48dc-b899-a6a3cced9b1d,https://data.globalchange.gov/reference/8c622c97-0a72-48dc-b899-a6a3cced9b1d,8c622c97-0a72-48dc-b899-a6a3cced9b1d,,"Smith, Joel B.; Richels, Richard; Miller, Barbara",,,,,219-249,"Potential consequences of climate variaility and change for the western United States",,2001,7,23920,8c622c97-0a72-48dc-b899-a6a3cced9b1d,"Book Section",/report/climate-change-impacts-on-united-states-potential-consequences-climate-variability-change-report-us-global-change-research-program
/reference/8ca4a4ae-9b6c-478f-bfc9-16762726dfff,https://data.globalchange.gov/reference/8ca4a4ae-9b6c-478f-bfc9-16762726dfff,8ca4a4ae-9b6c-478f-bfc9-16762726dfff,,"Xiao, Mu; Koppa, Akash; Mekonnen, Zelalem; Pagán, Brianna R.; Zhan, Shengan; Cao, Qian; Aierken, Abureli; Lee, Hyongki; Lettenmaier, Dennis P.",10.1002/2017GL073333,,10,"Geophysical Research Letters",4872-4879,"How much groundwater did California's Central Valley lose during the 2012–2016 drought?",44,2017,,21388,8ca4a4ae-9b6c-478f-bfc9-16762726dfff,"Journal Article",/article/10.1002/2017GL073333
/reference/8ddfda37-f9e3-4848-aa97-6f5eb0704765,https://data.globalchange.gov/reference/8ddfda37-f9e3-4848-aa97-6f5eb0704765,8ddfda37-f9e3-4848-aa97-6f5eb0704765,,"Reid, Colleen E.; Mann, Jennifer K.; Alfasso, Ruth; English, Paul B.; King, Galatea C.; Lincoln, Rebecca A.; Margolis, Helene G.; Rubado, Dan J.; Sabato, Joseph E.; West, Nancy L.; Woods, Brian; Navarro, Kathleen M.; Balmes, J. R.",10.1289/ehp.1103766,,5,"Environmental Health Perspectives",715-720,"Evaluation of a heat vulnerability index on abnormally hot days: An environmental public health tracking study",120,2012,0,4227,8ddfda37-f9e3-4848-aa97-6f5eb0704765,"Journal Article",/article/10.1289/ehp.1103766
/reference/8dfecf8b-f8a8-4f03-8d68-551b13794a1d,https://data.globalchange.gov/reference/8dfecf8b-f8a8-4f03-8d68-551b13794a1d,8dfecf8b-f8a8-4f03-8d68-551b13794a1d,,"Westerling, A.L.
Bryant, B.P.
Preisler, H.K.
Holmes, T.P.
Hidalgo, H.G.
Das, T.
Shrestha, S.R.",10.1007/s10584-011-0329-9,,"1 supplement","Climatic Change",445-463,"Climate change and growth scenarios for California wildfire",109,2011,0,3395,8dfecf8b-f8a8-4f03-8d68-551b13794a1d,"Journal Article",/article/10.1007/s10584-011-0329-9
/reference/8e18883e-9d45-4998-a0dd-bf59bab323ad,https://data.globalchange.gov/reference/8e18883e-9d45-4998-a0dd-bf59bab323ad,8e18883e-9d45-4998-a0dd-bf59bab323ad,"Large changes in the hydrology of the western United States have been observed since the mid-twentieth century. These include a reduction in the amount of precipitation arriving as snow, a decline in snowpack at low and midelevations, and a shift toward earlier arrival of both snowmelt and the centroid (center of mass) of streamflows. To project future water supply reliability, it is crucial to obtain a better understanding of the underlying cause or causes for these changes. A regional warming is often posited as the cause of these changes without formal testing of different competitive explanations for the warming. In this study, a rigorous detection and attribution analysis is performed to determine the causes of the late winter/early spring changes in hydrologically relevant temperature variables over mountain ranges of the western United States. Natural internal climate variability, as estimated from two long control climate model simulations, is insufficient to explain the rapid increase in daily minimum and maximum temperatures, the sharp decline in frost days, and the rise in degree-days above 0°C (a simple proxy for temperature-driven snowmelt). These observed changes are also inconsistent with the model-predicted responses to variability in solar irradiance and volcanic activity. The observations are consistent with climate simulations that include the combined effects of anthropogenic greenhouse gases and aerosols. It is found that, for each temperature variable considered, an anthropogenic signal is identifiable in observational fields. The results are robust to uncertainties in model-estimated fingerprints and natural variability noise, to the choice of statistical downscaling method, and to various processing options in the detection and attribution method.","Bonfils, C.
Santer, B.D.
Pierce, D.W.
Hidalgo, H.G.
Bala, G.
Das, T.
Barnett, T.P.
Cayan, D.R.
Doutriaux, C.
Wood, A.W.
Mirin, A.
Nozawa, T.",10.1175/2008JCLI2397.1,,23,"Journal of Climate",6404-6424,"Detection and attribution of temperature changes in the mountainous western United States",21,2008,0,507,8e18883e-9d45-4998-a0dd-bf59bab323ad,"Journal Article",/article/10.1175/2008JCLI2397.1
/reference/8e1ab38d-5d31-4a6a-8ad6-e06fe74a4aa1,https://data.globalchange.gov/reference/8e1ab38d-5d31-4a6a-8ad6-e06fe74a4aa1,8e1ab38d-5d31-4a6a-8ad6-e06fe74a4aa1,,"NOAA,",,,,,,"Mean sea level trend: 9414290 San Francisco, California",,2017,16,23931,8e1ab38d-5d31-4a6a-8ad6-e06fe74a4aa1,"Web Page",/webpage/92fcc83c-c31a-46b0-bdd7-99a9070bdda7
/reference/8e56543a-5a74-43e9-9ce5-a4170e5b3dde,https://data.globalchange.gov/reference/8e56543a-5a74-43e9-9ce5-a4170e5b3dde,8e56543a-5a74-43e9-9ce5-a4170e5b3dde,,"Balch, Jennifer K.; Bradley, Bethany A.; D'Antonio, Carla M.; Gómez-Dans, José",10.1111/gcb.12046,,1,"Global Change Biology",173-183,"Introduced annual grass increases regional fire activity across the arid western USA (1980–2009)",19,2013,,23717,8e56543a-5a74-43e9-9ce5-a4170e5b3dde,"Journal Article",/article/10.1111/gcb.12046
/reference/8e91f42b-50a5-4b30-a4ce-445f836056c6,https://data.globalchange.gov/reference/8e91f42b-50a5-4b30-a4ce-445f836056c6,8e91f42b-50a5-4b30-a4ce-445f836056c6,,"Anderson, Dean M.; Estell, Rick E.; Gonzalez, Alfredo L.; Cibils, Andres F.; Torell, L. Allen",10.1016/j.rala.2015.01.006,2015/04/01/,2,Rangelands,62-67,"Criollo cattle: Heritage genetics for arid landscapes",37,2015,,23711,8e91f42b-50a5-4b30-a4ce-445f836056c6,"Journal Article",/article/10.1016/j.rala.2015.01.006
/reference/8ebd54b0-fa0c-4cf5-8aa3-4ed7504f2add,https://data.globalchange.gov/reference/8ebd54b0-fa0c-4cf5-8aa3-4ed7504f2add,8ebd54b0-fa0c-4cf5-8aa3-4ed7504f2add,,"Lehner, Flavio; Wahl, Eugene R.; Wood, Andrew W.; Blatchford, Douglas B.; Llewellyn, Dagmar",10.1002/2017GL073253,,9,"Geophysical Research Letters",4124-4133,"Assessing recent declines in Upper Rio Grande runoff efficiency from a paleoclimate perspective",44,2017,,23809,8ebd54b0-fa0c-4cf5-8aa3-4ed7504f2add,"Journal Article",/article/10.1002/2017GL073253
/reference/8f6a7a67-ce7a-4462-a9fb-74308ac28013,https://data.globalchange.gov/reference/8f6a7a67-ce7a-4462-a9fb-74308ac28013,8f6a7a67-ce7a-4462-a9fb-74308ac28013,,"CARB,",,,,,20,"California greenhouse gas emissions for 2000 to 2016: Trends of emissions and other indicators",,2018,10,26388,8f6a7a67-ce7a-4462-a9fb-74308ac28013,Report,/report/california-greenhouse-gas-emissions-2000-2016-trends-emissions-other-indicators
/reference/8ff328a4-9570-4e27-8dbd-97db149d22dc,https://data.globalchange.gov/reference/8ff328a4-9570-4e27-8dbd-97db149d22dc,8ff328a4-9570-4e27-8dbd-97db149d22dc,"Santa Ana Winds (SAWs) are an integral feature of the regional climate of Southern California/Northern Baja California region, but their climate-scale behavior is poorly understood. In the present work, we identify SAWs in mesoscale dynamical downscaling of a global reanalysis from 1948 to 2012. Model winds are validated with anemometer observations. SAWs exhibit an organized pattern with strongest easterly winds on westward facing downwind slopes and muted magnitudes at sea and over desert lowlands. We construct hourly local and regional SAW indices and analyze elements of their behavior on daily, annual, and multidecadal timescales. SAWs occurrences peak in winter, but some of the strongest winds have occurred in fall. Finally, we observe that SAW intensity is influenced by prominent large-scale low-frequency modes of climate variability rooted in the tropical and north Pacific ocean-atmosphere system.","Guzman-Morales, Janin; Gershunov, Alexander; Theiss, Jurgen; Li, Haiqin; Cayan, Daniel",10.1002/2016GL067887,,6,"Geophysical Research Letters",2827-2834,"Santa Ana winds of Southern California: Their climatology, extremes, and behavior spanning six and a half decades",43,2016,,26362,8ff328a4-9570-4e27-8dbd-97db149d22dc,"Journal Article",/article/10.1002/2016GL067887
/reference/9018c683-2c96-4424-a01b-973fd5bd1626,https://data.globalchange.gov/reference/9018c683-2c96-4424-a01b-973fd5bd1626,9018c683-2c96-4424-a01b-973fd5bd1626,,"Gershunov, Alexander
Cayan, Daniel R.
Iacobellis, Sam F.",10.1175/2009jcli2465.1,2009/12/01,23,"Journal of Climate",6181-6203,"The great 2006 heat wave over California and Nevada: Signal of an increasing trend",22,2009,0,799,9018c683-2c96-4424-a01b-973fd5bd1626,"Journal Article",/article/10.1175/2009jcli2465.1
/reference/90a2ffd1-1b04-4e85-9bc1-7b9778858c50,https://data.globalchange.gov/reference/90a2ffd1-1b04-4e85-9bc1-7b9778858c50,90a2ffd1-1b04-4e85-9bc1-7b9778858c50,,"Wotkyns, Susan",,"September 13-14",,,31,"Workshop Report",,,,26403,90a2ffd1-1b04-4e85-9bc1-7b9778858c50,"Conference Proceedings",/generic/efa5ba3f-09d3-4c73-9dc7-9029111c0544
/reference/9155f29a-6970-44fe-b4ac-64253784e5e0,https://data.globalchange.gov/reference/9155f29a-6970-44fe-b4ac-64253784e5e0,9155f29a-6970-44fe-b4ac-64253784e5e0,,"Goode, Ron W.",,,,,5,"Burning Down to the Village",,2013,10,23951,9155f29a-6970-44fe-b4ac-64253784e5e0,Report,/report/burning-down-village
/reference/919be859-ff09-4c3a-89c8-72433add7e42,https://data.globalchange.gov/reference/919be859-ff09-4c3a-89c8-72433add7e42,919be859-ff09-4c3a-89c8-72433add7e42,"Purpose Heat waves could reveal or aggravate several ‘serious’ adverse drug reactions (ADRs) in elderly. Thus, we wanted to describe the main characteristics of heat-related ‘serious’ ADRs occurred in patients older than 70 years during these two events in France (2003 and 2006). Methods We analysed ‘serious’ ADRs reported to the network of French pharmacovigilance centres in summer 2003 and 2006 and suspected to be heat related. ‘Serious’ ADRs occurred during summers with heat waves (2003 and 2006) were compared with ADRs occurred during the same months in the summers of 2004 and 2005 (reference period). Results Patients' characteristics and number of ‘serious’ ADRs were similar whatever the year of the study. Number of drug-related deaths seemed higher in 2003 than in 2004–2005. More ‘serious’ heat-related ADRs were reported in the summers of 2003 and 2006 (68 in 2003 and 72 in 2006). Comparing with the reference period, metabolic ADRs were less frequent during the summers of 2003 (29%, p = 0.0001) and 2006 (39%, p = 0.003). Occurrence of other ADRs was similar whatever the period. Drugs more frequently involved during heat waves were diuretics, serotonic antidepressants, angiotensin converting inhibitors and proton pump inhibitors. Differences between 2003 and 2006 were found for non-dopaminergic (atropinic) antiparkinsonians or antiepileptics (most frequently involved in 2006) and beta-blockers or proton pump inhibitors (less frequently involved in 2006). Conclusion The present study underlines the interest of a National Pharmacovigilance Database to follow each year the role of drugs in heat-related ADRs. This survey should be associated with other pharmacoepidemiological methods, such as case–control or population-based studies. Copyright © 2011 John Wiley & Sons, Ltd.","Sommet, Agnès; Durrieu, Genevieve; Lapeyre-Mestre, Maryse; Montastruc, Jean-Louis",10.1002/pds.2307,,3,"Pharmacoepidemiology and Drug Safety",285-288,"A comparative study of adverse drug reactions during two heat waves that occurred in France in 2003 and 2006",21,2012,,25984,919be859-ff09-4c3a-89c8-72433add7e42,"Journal Article",/article/10.1002/pds.2307
/reference/91a0e8e7-a505-4c42-a957-c999b2a25c38,https://data.globalchange.gov/reference/91a0e8e7-a505-4c42-a957-c999b2a25c38,91a0e8e7-a505-4c42-a957-c999b2a25c38,,"Hohner, Amanda K.; Cawley, Kaelin; Oropeza, Jill; Summers, R. Scott; Rosario-Ortiz, Fernando L.",10.1016/j.watres.2016.08.034,2016/11/15/,,"Water Research",187-198,"Drinking water treatment response following a Colorado wildfire",105,2016,,23780,91a0e8e7-a505-4c42-a957-c999b2a25c38,"Journal Article",/article/10.1016/j.watres.2016.08.034
/reference/92b75533-4ebe-4cad-af48-6789b4627f47,https://data.globalchange.gov/reference/92b75533-4ebe-4cad-af48-6789b4627f47,92b75533-4ebe-4cad-af48-6789b4627f47,,"DOE,",,,,,84,"U.S. energy and employment report",,2017,10,26402,92b75533-4ebe-4cad-af48-6789b4627f47,Report,/report/us-energy-employment-report
/reference/92c5f606-3032-4d7b-9356-3b65de47cf14,https://data.globalchange.gov/reference/92c5f606-3032-4d7b-9356-3b65de47cf14,92c5f606-3032-4d7b-9356-3b65de47cf14,,"Musselman, Keith N.; Clark, Martyn P.; Liu, Changhai; Ikeda, Kyoko; Rasmussen, Roy",10.1038/nclimate3225,02/27/online,,"Nature Climate Change",214-219,"Slower snowmelt in a warmer world",7,2017,,26348,92c5f606-3032-4d7b-9356-3b65de47cf14,"Journal Article",/article/10.1038/nclimate3225
/reference/92ef48b3-a700-46f9-9762-461c83b6dca8,https://data.globalchange.gov/reference/92ef48b3-a700-46f9-9762-461c83b6dca8,92ef48b3-a700-46f9-9762-461c83b6dca8,,"Sloan, Kathleen; Hostler, Joe",,,,,17,"Utilizing Yurok Traditional Ecological Knowledge to Inform Climate Change Priorities",,2014,10,23921,92ef48b3-a700-46f9-9762-461c83b6dca8,Report,/report/utilizing-yurok-traditional-ecological-knowledge-inform-climate-change-priorities
/reference/9333b491-96fb-40a1-a777-8f3000aa1354,https://data.globalchange.gov/reference/9333b491-96fb-40a1-a777-8f3000aa1354,9333b491-96fb-40a1-a777-8f3000aa1354,"California’s climate is characterized by the largest precipitation and streamflow variability observed within the conterminous US This, combined with chronic groundwater overdraft of 0.6–3.5 km 3 yr −1 , creates the need to identify additional surface water sources available for groundwater recharge using methods such as agricultural groundwater banking, aquifer storage and recovery, and spreading basins. High-magnitude streamflow, i.e. flow above the 90th percentile, that exceeds environmental flow requirements and current surface water allocations under California water rights, could be a viable source of surface water for groundwater banking. Here, we present a comprehensive analysis of the magnitude, frequency, duration and timing of high-magnitude streamflow (HMF) for 93 stream gauges covering the Sacramento, San Joaquin and Tulare basins in California. The results show that in an average year with HMF approximately 3.2 km 3 of high-magnitude flow is exported from the entire Central Valley to the Sacramento-San Joaquin Delta often at times when environmental flow requirements of the Delta and major rivers are exceeded. High-magnitude flow occurs, on average, during 7 and 4.7 out of 10 years in the Sacramento River and the San Joaquin-Tulare Basins, respectively, from just a few storm events (5–7 1-day peak events) lasting for 25–30 days between November and April. The results suggest that there is sufficient unmanaged surface water physically available to mitigate long-term groundwater overdraft in the Central Valley.","Kocis, Tiffany N.; Helen E. Dahlke",10.1088/1748-9326/aa7b1b,,8,"Environmental Research Letters",084009,"Availability of high-magnitude streamflow for groundwater banking in the Central Valley, California",12,2017,,23680,9333b491-96fb-40a1-a777-8f3000aa1354,"Journal Article",/article/10.1088/1748-9326/aa7b1b