Ag in Drought

Total Page:16

File Type:pdf, Size:1020Kb

Load more

Percent of Barley Located in Drought September 14, 2021 100 100 100 100 100 100 100 100 97 98 4 91 10 14 90 87 24 35 9 80 19 70 55 68 60 78 77 33 36 50 86 98 Percent 90 40 52 65 30 5 27 36 20 36 17 20 28 10 14 18 6 3 6 2 21 Utah (1) Texas (1) Maine (1) Idaho (31) Virginia (1) Oregon (1) Arizona (1) Colorado (5) Maryland (1) Wyoming(4) California (2) Delaware (1) Montana (20) UnitedStates Minnesota(3) Washington (3) Pennsylvania (2) NorthDakota (18) Drought percentages are approximated Percent in Moderate Drought (D1) Percent in Severe Drought (D2) using the U.S. Drought Monitor product. State contributions to national production Percent in Extreme Drought (D3) Percent in Exceptional Drought (D4) (percentages in parentheses) are derived from NASS 2017 Census of Agriculture data. Percent of United States Barley Located in Drought 100 8888 90 87878787 87 8384 8080 80 72 7171 7070 706969 70 62 62 63 595959 59 57 57 58 60 55 5555 55 52 5353 52 51 50 484848 48 50 46 47 46 464747 4444 444444 43 42 43 42 Percent 41 41 4041 40 41 39 393839 39 39 40 36 3536 3232 2929 2930 28 28 2828 27 30 25 2626 22222222222323 22 22 2323 22 222322 21 2120202020 21 20202020 21 18 191919 18 1919 20 16 16 17 17 141515 15 1414 12 13 13 10 10 8 8 9 9 9 10 6 6 7 7 7 7 7 6 7 7 7 7 7 6 6 6 6 6 6 6 6 5 4 4 4 5 5 5 5 5 5 5 4 4 4 5 1 1 1 1 1 1 1 1 2 2 2 2 2 2 2 2 2 2 2 1 1 1 1 1 1 1 2 2 2 2 2 2 0 Jul 6 2021 Oct6 2020 Apr6 2021 Jan Jan 52021 Jun 12021 Jun 82021 Feb 9 2021 Feb 2 2021 Mar 2 2021 Mar 9 2021 Nov3 2020 Dec1 2020 Dec8 2020 Aug3 2021 Sep7 2021 Jul 202127 Jul 202113 Jul 202120 May 4 2021 Apr20 2021 Apr27 2021 Oct13 2020 Oct20 2020 Oct27 2020 Apr13 2021 Jan 12 2021 Jun 22 2021 Jun 29 2021 Jan 19 2021 Jan 26 2021 Jun 15 2021 Feb 202116 Mar 202116 Mar 202123 Feb 202123 Mar 202130 Nov10 2020 Dec15 2020 Nov17 2020 Nov24 2020 Dec22 2020 Dec29 2020 Sep29 2020 Aug31 2021 Sep15 2020 Sep22 2020 Aug10 2021 Aug17 2021 Aug24 2021 Sep14 2021 May 202118 May 202125 May 202111 Moderate or more intense drought (D1+) Severe or more intense drought (D2+) Drought percentages are approximated Extreme or more intense drought (D3+) Exceptional drought (D4) using the U.S. Drought Monitor product. Percent of Corn Located in Drought September 14, 2021 100 100 90 33 80 75 69 70 7 3 60 13 51 50 43 38 Percent 11 40 30 30 30 2 7 53 8 20 41 17 13 2 29 10 25 10 23 7 21 3 5 6 13 15 1 8 5 6 6 Ohio (4) Iowa (17) Texas (2) Indiana(7) Illinois (15) Kansas (5) Missouri(4) Michigan (2) Colorado (1) Kentucky (1) Arkansas(1) Louisiana (1) NewYork(1) UnitedStates Wisconsin(4) Mississippi (1) Nebraska (11) Tennessee (1) Minnesota(10) NorthDakota (3) Pennsylvania (1) South Dakota(5) NorthCarolina (1) Drought percentages are approximated Percent in Moderate Drought (D1) Percent in Severe Drought (D2) using the U.S. Drought Monitor product. State contributions to national production Percent in Extreme Drought (D3) Percent in Exceptional Drought (D4) (percentages in parentheses) are derived from NASS 2017 Census of Agriculture data. Percent of United States Corn Located in Drought 100 90 80 70 60 50 Percent 4141 39 37373738 3838 37 3738 40 36 363536363636 36363635 35 363636 35 32 32 32 30 31 3030 28 29 30 2727 26 2324 24242424 2424 21 22 2122 22 2221 201919 191920 17 17 1717 18 20 1616 16 15151515 13131414 141414 13 121212 11 9 9 10 9 9 9 10 9 9 1010 7 7 7 7 7 7 7 8 10 5 5 5 6 6 6 5 5 5 5 5 5 6 6 6 5 6 6 3 3 3 3 3 3 4 4 4 4 4 3 3 1 1 1 2 1 1 1 2 2 2 2 2 2 2 1 1 1 2 2 2 2 2 2 1 1 1 1 1 2 0 Jul 6 2021 Oct6 2020 Apr6 2021 Jan Jan 52021 Jun 12021 Jun 82021 Feb 9 2021 Feb 2 2021 Mar 2 2021 Mar 9 2021 Nov3 2020 Dec1 2020 Dec8 2020 Aug3 2021 Sep7 2021 Jul 202127 Jul 202113 Jul 202120 May 4 2021 Apr20 2021 Apr27 2021 Oct13 2020 Oct20 2020 Oct27 2020 Apr13 2021 Jan 12 2021 Jun 22 2021 Jun 29 2021 Jan 19 2021 Jan 26 2021 Jun 15 2021 Feb 202116 Mar 202116 Mar 202123 Feb 202123 Mar 202130 Nov10 2020 Dec15 2020 Nov17 2020 Nov24 2020 Dec22 2020 Dec29 2020 Sep29 2020 Aug31 2021 Sep15 2020 Sep22 2020 Aug10 2021 Aug17 2021 Aug24 2021 Sep14 2021 May 202118 May 202125 May 202111 Moderate or more intense drought (D1+) Severe or more intense drought (D2+) Drought percentages are approximated Extreme or more intense drought (D3+) Exceptional drought (D4) using the U.S. Drought Monitor product. Percent of Cotton Located in Drought September 14, 2021 100 100 92 90 80 70 60 92 50 Percent 92 40 30 19 20 10 10 19 4 5 8 10 1 4 4 Florida(1) Texas (45) Kansas (1) Virginia (1) Arizona (2) Missouri(4) Alabama(4) Georgia (11) Arkansas(5) California (1) Louisiana (2) UnitedStates Oklahoma(5) Mississippi (7) Tennessee (4) NewMexico (1) NorthCarolina (4) South Carolina (2) Drought percentages are approximated Percent in Moderate Drought (D1) Percent in Severe Drought (D2) using the U.S. Drought Monitor product. State contributions to national production Percent in Extreme Drought (D3) Percent in Exceptional Drought (D4) (percentages in parentheses) are derived from NASS 2017 Census of Agriculture data. Percent of United States Cotton Located in Drought 100 90 80 70 60 50 45 4242 4242 Percent 41 41 4141 3939383938 40 36 36 3636 37 34 34 35 33 3233 333233 333333 32 3130 3030 31 2828 28 30 2626 2727 27 262627272726272626 26 242525 242425 25252524252424 2424 22 2222 23 21 202121 202021202021 19 19 191919 18181818181819 20 161616161515 15 14 14 1414 14131413 1111 1111 12 9 9 9 9 9 9 9 9 9 9 9 9 9 9 9 9 9 7 7 8 8 8 8 8 7 10 5 5 5 5 5 5 5 5 6 5 5 5 3 3 3 4 4 4 34 34 34 34 34 34 34 4 4 4 4 2 2 2 2 2 2 1 12 1 1 12 12 12 1 1 0 Jul 6 2021 Oct6 2020 Apr6 2021 Jan Jan 52021 Jun 12021 Jun 82021 Feb 9 2021 Feb 2 2021 Mar 2 2021 Mar 9 2021 Nov3 2020 Dec1 2020 Dec8 2020 Aug3 2021 Sep7 2021 Jul 202127 Jul 202113 Jul 202120 May 4 2021 Apr20 2021 Apr27 2021 Oct13 2020 Oct20 2020 Oct27 2020 Apr13 2021 Jan 12 2021 Jun 22 2021 Jun 29 2021 Jan 19 2021 Jan 26 2021 Jun 15 2021 Feb 202116 Mar 202116 Mar 202123 Feb 202123 Mar 202130 Nov10 2020 Dec15 2020 Nov17 2020 Nov24 2020 Dec22 2020 Dec29 2020 Sep29 2020 Aug31 2021 Sep15 2020 Sep22 2020 Aug10 2021 Aug17 2021 Aug24 2021 Sep14 2021 May 202118 May 202125 May 202111 Moderate or more intense drought (D1+) Severe or more intense drought (D2+) Drought percentages are approximated Extreme or more intense drought (D3+) Exceptional drought (D4) using the U.S. Drought Monitor product. Percent of Peanuts Located in Drought September 14, 2021 100 90 80 70 60 50 Percent 40 30 20 10 Texas (9) Florida(9) Virginia (2) Georgia (50) Arkansas(2) Alabama(10) UnitedStates Oklahoma(1) Mississippi (2) NorthCarolina (7) South Carolina (7) Drought percentages are approximated Percent in Moderate Drought (D1) Percent in Severe Drought (D2) using the U.S. Drought Monitor product. State contributions to national production Percent in Extreme Drought (D3) Percent in Exceptional Drought (D4) (percentages in parentheses) are derived from NASS 2017 Census of Agriculture data. Percent of United States Peanuts Located in Drought 100 90 80 70 60 50 Percent 40 30 2120 20 11 1111 1211 9 9 9 10109 109 109 109 109 109 109 109 109 109 109 109 109 109 109 109 109 9 1010109 9 9 109 109 109 109 109 109 9 9 8 8 8 8 7 7 7 7 7 7 8 8 8 8 8 8 7 7 7 7 7 7 78 78 7 7 7 7 7 7 7 7 7 8 7 7 7 10 5 5 56 56 5 5 5 5 5 6 6 6 6 6 6 6 6 6 6 6 3 3 34 34 3 3 4 1 1 1 1 1 1 1 1 1 1 1 1 0 Jul 6 2021 Oct6 2020 Apr6 2021 Jan Jan 52021 Jun 12021 Jun 82021 Feb 9 2021 Feb 2 2021 Mar 2 2021 Mar 9 2021 Nov3 2020 Dec1 2020 Dec8 2020 Aug3 2021 Sep7 2021 Jul 202127 Jul 202113 Jul 202120 May 4 2021 Apr20 2021 Apr27 2021 Oct13 2020 Oct20 2020 Oct27 2020 Apr13 2021 Jan 12 2021 Jun 22 2021 Jun 29 2021 Jan 19 2021 Jan 26 2021 Jun 15 2021 Feb 202116 Mar 202116 Mar 202123 Feb 202123 Mar 202130 Nov10 2020 Dec15 2020 Nov17 2020 Nov24 2020 Dec22 2020 Dec29 2020 Sep29 2020 Aug31 2021 Sep15 2020 Sep22 2020 Aug10 2021 Aug17 2021 Aug24 2021 Sep14 2021 May 202118 May 202125 May 202111 Moderate or more intense drought (D1+) Severe or more intense drought (D2+) Drought percentages are approximated Extreme or more intense drought (D3+) Exceptional drought (D4) using the U.S.
Recommended publications
  • Climate Change and Water Management in South Florida

    Climate Change and Water Management in South Florida

    Interdepartmental Climate Change Group District Leadership Team Subteam: Kenneth Ammon Deena Reppen Sharon Trost Interdepartmental Climate Change Group Members: Wossenu Abtew Chandra Pathak Restoration Sciences SCADA & Hydrological Data Management Matahel Ansar Christopher Pettit Operations & Maintenance Office of Counsel Jenifer Barnes Barbara Powell Hydrologic & Environmental Systems Water Supply Modeling Dean Powell Luis Cadavid Water Supply Hydrologic & Environmental Systems Angela Prymas Modeling Regulation James Carnes Garth Redfield Intergovernmental Programs Restoration Sciences Tibebe Dessalegne-Agaze Keith Rizzardi BEM Systems Inc. (contractor) Office of Counsel Cynthia Gefvert Winifred Said Water Supply Hydrologic & Environmental Systems Lawrence Gerry Modeling Everglades Restoration Natalie Schneider Linda Hoppes Intergovernmental Programs Water Supply Bruce Sharfstein Michelle Irizarry-Ortiz Restoration Sciences Hydrologic & Environmental Systems Modeling Kim Shugar Intergovernmental Programs Jeremy McBryan Restoration Sciences Fred Sklar Restoration Sciences Damon Meiers Intergovernmental Programs Paul Trimble Hydrologic & Environmental Systems John Morgan Modeling Intergovernmental Programs Bob Verrastro John Mulliken Intergovernmental Programs Water Supply Patti Nicholas Dewey Worth Public Information Everglades Restoration Jayantha Obeysekera Nathan Yates Hydrologic & Environmental Systems Restoration Sciences Modeling i Table of Contents Executive Summary ................................................................................................
  • Global Warming Impacts on Severe Drought Characteristics in Asia Monsoon Region

    Global Warming Impacts on Severe Drought Characteristics in Asia Monsoon Region

    water Article Global Warming Impacts on Severe Drought Characteristics in Asia Monsoon Region Jeong-Bae Kim , Jae-Min So and Deg-Hyo Bae * Department of Civil & Environmental Engineering, Sejong University, 209 Neungdong-ro, Gwangjin-Gu, Seoul 05006, Korea; [email protected] (J.-B.K.); [email protected] (J.-M.S.) * Correspondence: [email protected]; Tel.: +82-2-3408-3814 Received: 2 April 2020; Accepted: 7 May 2020; Published: 12 May 2020 Abstract: Climate change influences the changes in drought features. This study assesses the changes in severe drought characteristics over the Asian monsoon region responding to 1.5 and 2.0 ◦C of global average temperature increases above preindustrial levels. Based on the selected 5 global climate models, the drought characteristics are analyzed according to different regional climate zones using the standardized precipitation index. Under global warming, the severity and frequency of severe drought (i.e., SPI < 1.5) are modulated by the changes in seasonal and regional precipitation − features regardless of the region. Due to the different regional change trends, global warming is likely to aggravate (or alleviate) severe drought in warm (or dry/cold) climate zones. For seasonal analysis, the ranges of changes in drought severity (and frequency) are 11.5%~6.1% (and 57.1%~23.2%) − − under 1.5 and 2.0 ◦C of warming compared to reference condition. The significant decreases in drought frequency are indicated in all climate zones due to the increasing precipitation tendency. In general, drought features under global warming closely tend to be affected by the changes in the amount of precipitation as well as the changes in dry spell length.
  • Additional Arrangements for Drought Under the UNCCD Prospective Assessment

    Additional Arrangements for Drought Under the UNCCD Prospective Assessment

    Additional arrangements for drought under the UNCCD Prospective assessment April 2019 This prospective assessment concerning additional arrangements for drought under the UNCCD looks at a variety of legal instruments of international cooperation, ranging from protocols to gentleman’s agreements, and assesses their suitability for addressing drought under the UNCCD. The assessment uses information of experiences in using these tools under other international processes, and takes into account the specific priorities and working modalities of the Convention in addressing drought. On this basis, the assessment presents conclusions on the likelihood of success of each legal instrument in addressing drought under the UNCCD. This assessment was authored by the UNCCD Evaluation Office with the support of Dr. Sylvestre- José-Tidiane Manga and Ms. Aurore Vernhes in June 2018 – April 2019. 2 Additional arrangements for drought under the UNCCD: a prospective assessment List of content Page 1. Introduction 5 2. Drought in the context of international cooperation 6 2.1 About drought 6 2.2 Addressing drought through international cooperation 7 2.3 Addressing drought in the context of the UNCCD 9 3. Potential legal instruments for addressing drought under the UNCCD 10 3.1 An overview of legal instruments for international environmental 10 cooperation 3.2 Legal instruments 12 a) Protocols 12 b) Annexes and amendments 19 c) Principles 22 d) Declarations 26 e) Decisions 29 f) Standards 31 g) Gentlemen’s Agreements 34 4. Conclusions 36 Annex: Potential legal
  • Climate Change and Drought

    Climate Change and Drought

    Climate Change and Drought What it means to tribes and how we can adapt What is drought? These two issues in concert present serious questions The National Oceanic and Atmospheric Administration about water availability and access into the future. (NOAA) defines drought as “a deficiency in precipitation Quick facts about drought in the Southwest: over an extended period, usually a season or more, The Southwest has been in a consistent state of resulting in a water shortage causing adverse impacts on drought since 1999. vegetation, animals, and/or people[1]”. The West has Historical drought trends along with projected often suffered from extensive drought periods including temperature increases suggest that droughts will some of the longest drought events on Earth - so called become even more severe over time. mega-droughts[2]. As global temperatures rise due to climate change, areas such as the Southwest are likely Reconstructed drought trends (assembled from to experience “increasing and deepening drought tree ring data) indicate longer drought patterns conditions[3]”. This could have devastating effects on over the last 100 years than previously observed. water supply for ecosystems, agriculture, and for human Winter and spring storm tracks, which bring annual consumption. regional rain, are projected to shift northward. What are the facts? Over the last century the average global temperature has increased by approximately 1.2° C (2.2° F)[4]. Comprehensive, long-term research by governmental agencies and academic institutions indicates that this temperature increase is directly linked to human activities - specifically large-scale greenhouse gas emissions. This human-induced, or anthropogenic, temperature change is causing variable global and Prolonged drought conditions can cause severe damage regional climatic effects.
  • Ramping up Reforestation in the United States: a Guide for Policymakers March 2021 Cover Photo: CDC Photography / American Forests

    Ramping up Reforestation in the United States: a Guide for Policymakers March 2021 Cover Photo: CDC Photography / American Forests

    Ramping up Reforestation in the United States: A Guide for Policymakers March 2021 Cover photo: CDC Photography / American Forests Executive Summary Ramping Up Reforestation in the United States: A Guide for Policymakers is designed to support the development of reforestation policies and programs. The guide highlights key findings on the state of America’s tree nursery infrastructure and provides a range of strategies for encouraging and enabling nurseries to scale up seedling production. The guide builds on a nationwide reforestation assessment (Fargione et al., 2021) and follow-on assessments (Ramping Up Reforestation in the United States: Regional Summaries companion guide) of seven regions in the contiguous United States (Figure 1). Nursery professionals throughout the country informed our key findings and strategies through a set of structured interviews and a survey. Across the contiguous U.S., there are over 133 million acres of reforestation opportunity on lands that have historically been forested (Cook-Patton et al., 2020). This massive reforestation opportunity equals around 68 billion trees. The majority of opportunities occur on pastureland, including those with poor soils in the Eastern U.S. Additionally, substantial reforestation opportunities in the Western U.S. are driven by large, severe wildfires. Growing awareness of this potential has led governments and organizations to ramp up reforestation to meet ambitious climate and biodiversity goals. Yet, there are many questions about the ability of nurseries to meet the resulting increase in demand for tree seedlings. These include a lack of seed, workforce constraints, and insufficient nursery infrastructure. To meet half of the total reforestation opportunity by 2040 (i.e., 66 million acres) would require America’s nurseries to produce an additional 1.8 billion seedlings each year.
  • Climate, Drought, and Sea Level Rise Scenarios for California's Fourth

    Climate, Drought, and Sea Level Rise Scenarios for California's Fourth

    CLIMATE, DROUGHT, AND SEA LEVEL RISE SCENARIOS FOR CALIFORNIA’S FOURTH CLIMATE CHANGE ASSESSMENT A Report for: California’s Fourth Climate Change Assessment Prepared By: David W. Pierce1 Julie F. Kalansky1 1 Daniel R. Cayan 1 Division of Climate, Atmospheric Sciences, and Physical Oceanography Scripps Institution of Oceanography, La Jolla, California DISCLAIMER This report was prepared as the result of work sponsored by the California Energy Commission. It does not necessarily represent the views of the Energy Commission, its employees or the State of California. The Energy Commission, the State of California, its employees, contractors and subcontractors make no warrant, express or implied, and assume no legal liability for the information in this report; nor does any party represent that the uses of this information will not infringe upon privately owned rights. This report has not been approved or disapproved by the California Energy Commission nor has the California Energy Commission passed upon the accuracy or adequacy of the information in this report. August 2018 Edmund G. Brown, Jr., Governor CCCA4-CEC-2018-006 ACKNOWLEDGEMENTS We acknowledge the World Climate Research Programme's Working Group on Coupled Modelling, which is responsible for the Climate Model Intercomparison Project (CMIP), and we thank the climate modeling groups for producing and making available their model output. For CMIP the U.S. Department of Energy's Program for Climate Model Diagnosis and Intercomparison provides coordinating support and led development of software infrastructure in partnership with the Global Organization for Earth System Science Portals. This work was supported by the California Energy Commission, Agreement Number 500-14-005.
  • Improving Drought Management in the West: the Role of Mitigation and Preparedness

    Improving Drought Management in the West: the Role of Mitigation and Preparedness

    Utah State University DigitalCommons@USU U.S. Government Documents (Utah Regional Elusive Documents Depository) 1997 Improving Drought Management in the West: The Role of Mitigation and Preparedness Donald Wilhite Follow this and additional works at: https://digitalcommons.usu.edu/elusive_docs Part of the Environmental Sciences Commons Recommended Citation Wilhite, Donald, "Improving Drought Management in the West: The Role of Mitigation and Preparedness" (1997). Elusive Documents. Paper 71. https://digitalcommons.usu.edu/elusive_docs/71 This Book is brought to you for free and open access by the U.S. Government Documents (Utah Regional Depository) at DigitalCommons@USU. It has been accepted for inclusion in Elusive Documents by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. ( PB97204283 . 'n l 1111111111111111111111111111111 \.... IDlproving Drought ManagelTIent in the West The Role 'of Mitigation and Preparedness Donald Wilhite, Director National Drought Mitigation Center University of Nebraska I I PROTECTED UNDE '-- I ! ALL RIGHTS RESER~~~TERNATIONAL COPYRIGHT I i ~~:'g~'1;~~~~~ 6~~~~6~ON SERVICE I I Report to the Western Water Policy Review Advisory Commission June 1997 Contents Page Introduction .................................................... 1 The Concept of Drought. .. .. 2 Crisis Management Versus Risk Management Approach to Drought Management . .. .. 4 The Climatology of Drought in the West: 1895 to 1996 " . .. 6 The Climatology of Drought, 1986 to 1996 . .. 8 State-Level Drought Planning: Current Status ...................... 15 Lessons From Recent Droughts: State-Level Mitigation Tools .... .. 19 Integrating Drought Management and Water Policy .................. 25 Integrating Drought Management and Water Policy: New Directions. .. 36 Australian National Drought Policy: A Model for the United States? ............................................. ;..... 38 Conclusions and .Recommendations ...............................
  • What Climate Change Means for California

    What Climate Change Means for California

    August 2016 EPA 430-F-16-007 What Climate Change Means for California California’s climate is changing. Southern California Snowpack has warmed about three degrees (F) in the last century As the climate warms, less precipitation falls as snow, and more snow melts during and all of the state is becoming warmer. Heat waves the winter. That decreases snowpack—the amount of snow that accumulates are becoming more common, snow is melting earlier in over the winter. Since the 1950s, the snowpack has declined in California and the spring—and in southern California, less rain is falling nearby states that drain into the Colorado River. as well. In the coming decades, the changing climate is Diminishing snowpack can shorten the season for skiing and other forms of winter likely to further decrease the supply of water, increase tourism and recreation. The tree line may shift, as mountain hemlock and other the risk of wildfires, and threaten coastal development high-altitude trees become able to grow at higher elevations. A higher tree line and ecosystems. would decrease the extent of alpine tundra ecosystems, which could threaten some Our climate is changing because the earth is warming. species. People have increased the amount of carbon dioxide in the air by 40 percent since the late 1700s. Other Water Availability heat-trapping greenhouse gases are also increasing. The changing climate is likely to increase the need for water but reduce the supply. These gases have warmed the surface and lower Rising temperatures increase the rate at which water evaporates into the air from atmosphere of our planet about one degree during the soils and surface waters.
  • Ozone Depletion, Ultraviolet Radiation, Climate Change and Prospects for a Sustainable Future Paul W

    Ozone Depletion, Ultraviolet Radiation, Climate Change and Prospects for a Sustainable Future Paul W

    University of Wollongong Research Online Faculty of Science, Medicine and Health - Papers: Faculty of Science, Medicine and Health Part B 2019 Ozone depletion, ultraviolet radiation, climate change and prospects for a sustainable future Paul W. Barnes Loyola University New Orleans, [email protected] Craig E. Williamson United Nations Environment Programme, Environmental Effects Assessment Panel, Miami University, [email protected] Robyn M. Lucas Australian National University (ANU), United Nations Environment Programme, Environmental Effects Assessment Panel, University of Western Australia, [email protected] Sharon A. Robinson University of Wollongong, [email protected] Sasha Madronich United Nations Environment Programme, Environmental Effects Assessment Panel, National Center For Atmospheric Research, Boulder, United States, [email protected] See next page for additional authors Publication Details Barnes, P. W., Williamson, C. E., Lucas, R. M., Robinson, S. A., Madronich, S., Paul, N. D., Bornman, J. F., Bais, A. F., Sulzberger, B., Wilson, S. R., Andrady, A. L., McKenzie, R. L., Neale, P. J., Austin, A. T., Bernhard, G. H., Solomon, K. R., Neale, R. E., Young, P. J., Norval, M., Rhodes, L. E., Hylander, S., Rose, K. C., Longstreth, J., Aucamp, P. J., Ballare, C. L., Cory, R. M., Flint, S. D., de Gruijl, F. R., Hader, D. -P., Heikkila, A. M., Jansen, M. A.K., Pandey, K. K., Robson, T. Matthew., Sinclair, C. A., Wangberg, S., Worrest, R. C., Yazar, S., Young, A. R. & Zepp, R. G. (2019). Ozone depletion, ultraviolet radiation, climate change and prospects for a sustainable future. Nature Sustainability, Online First 1-11. Research Online is the open access institutional repository for the University of Wollongong.
  • Sea Level Rise and Implications for Low Lying Islands, Coasts And

    Sea Level Rise and Implications for Low Lying Islands, Coasts And

    SECOND ORDER DRAFT Chapter 4 IPCC SR Ocean and Cryosphere 1 2 Chapter 4: Sea Level Rise and Implications for Low Lying Islands, Coasts and Communities 3 4 Coordinating Lead Authors: Michael Oppenheimer (USA), Bruce Glavovic (New Zealand) 5 6 Lead Authors: Amro Abd-Elgawad (Egypt), Rongshuo Cai (China), Miguel Cifuentes-Jara (Costa Rica), 7 Rob Deconto (USA), Tuhin Ghosh (India), John Hay (Cook Islands), Jochen Hinkel (Germany), Federico 8 Isla (Argentina), Alexandre K. Magnan (France), Ben Marzeion (Germany), Benoit Meyssignac (France), 9 Zita Sebesvari (Hungary), AJ Smit (South Africa), Roderik van de Wal (Netherlands) 10 11 Contributing Authors: Maya Buchanan (USA), Gonéri Le Cozannet (France), Catia Domingues 12 (Australia), Petra Döll (Germany), Virginie K.E. Duvat (France), Tamsin Edwards (UK), Alexey Ekaykin 13 (Russian Federation), Miguel D. Fortes (Philippines), Thomas Frederikse (Netherlands), Jean-Pierre Gattuso 14 (France), Robert Kopp (USA), Erwin Lambert (Netherlands), Andrew Mackintosh (New Zealand), 15 Angélique Melet (France), Elizabeth McLeod (USA), Mark Merrifield (USA), Siddharth Narayan (US), 16 Robert J. Nicholls (UK), Fabrice Renaud (UK), Jonathan Simm (UK), Jon Woodruff (USA), Poh Poh Wong 17 (Singapore), Siyuan Xian (USA) 18 19 Review Editors: Ayako Abe-Ouchi (Japan), Kapil Gupta (India), Joy Pereira (Malaysia) 20 21 Chapter Scientist: Maya Buchanan (USA) 22 23 Date of Draft: 16 November 2018 24 25 Notes: TSU Compiled Version 26 27 28 Table of Contents 29 30 Executive Summary ......................................................................................................................................... 2 31 4.1 Purpose, Scope, and Structure of the Chapter ...................................................................................... 6 32 4.1.1 Themes of this Chapter ................................................................................................................... 6 33 4.1.2 Advances in this Chapter Beyond AR5 and SR1.5 ........................................................................
  • Glacier Albedo Reduction and Drought Effects in the Extratropical Andes, 1986–2020

    Glacier Albedo Reduction and Drought Effects in the Extratropical Andes, 1986–2020

    Journal of Glaciology Glacier albedo reduction and drought effects in the extratropical Andes, 1986–2020 Thomas E. Shaw1,2 , Genesis Ulloa3, David Farías-Barahona4, 3 3,5 2,6 Article Rodrigo Fernandez , Jose M. Lattus and James McPhee 1 2 Cite this article: Shaw TE, Ulloa G, Farías- Swiss Federal Institute for Forest, Snow and Landscape Research (WSL), Birmensdorf, Switzerland; Advanced Barahona D, Fernandez R, Lattus JM, McPhee J Mining Technology Center, Universidad de Chile, Santiago, Chile; 3Department of Geology, Universidad de Chile, (2021). Glacier albedo reduction and drought Santiago, Chile; 4Institute für Geographie, Friedrich-Alexander-Universität Erlangen-Nürnberg, Erlangen, Germany; effects in the extratropical Andes, 1986–2020. 5SRGIS: Geología y Geomática Ltda, Santiago, Chile and 6Department of Civil Engineering, Universidad de Chile, – Journal of Glaciology 67(261), 158 169. https:// Santiago, Chile doi.org/10.1017/jog.2020.102 Received: 10 August 2020 Abstract Revised: 10 November 2020 Surface albedo typically dominates the mass balance of mountain glaciers, though long-term Accepted: 11 November 2020 First published online: 17 December 2020 trends and patterns of glacier albedo are seldom explored. We calculated broadband shortwave albedo for glaciers in the central Chilean Andes (33–34°S) using end-of-summer Landsat scenes Key words: between 1986 and 2020. We found a high inter-annual variability of glacier-wide albedo that is Albedo; Andes; climate; drought; glacier; largely a function of the glacier fractional snow-covered area and the total precipitation of the remote sensing preceding hydrological year (up to 69% of the inter-annual variance explained). Under the Author for correspondence: 2010–2020 ‘Mega Drought’ period, the mean albedo, regionally averaged ranging from ∼0.25– Thomas E.
  • The International Crime of Ecocide the INTERNATIONAL CRIME of ECOCIDE

    The International Crime of Ecocide the INTERNATIONAL CRIME of ECOCIDE

    Gray: The International Crime of Ecocide THE INTERNATIONAL CRIME OF ECOCIDE MARK ALLAN GRAY* INTRODUCTION And I have felt A presence that disturbs me with the joy Of elevated thoughts; a sense sublime Of somethingfar more deeply interfused, Whose dwelling is the light of setting suns, And the round ocean and the living air, And the blue sky, and in the mind of man ...Therefore am I still A lover of the meadows and the woods, And mountains; and of all that we behold From this green earth William Wordsworth From earliest times, humans have demonstrated a remarkable capacity to subdue and alter their physical environment. What began as a struggle for survival became a predominance among living things, then, in wealthier societies, a relentless drive for comfort and pleasure. Even, perhaps especially, in less-developed countries (LDCs), where for many survival remains a struggle, the conquest of nature proceeds apace. "Development" is now a worldwide synonym for progress.' It is therefore ironic that the scope and effects of human activity actually threaten our survival as a species. Scientists and politicians cannot agree on the precise causes and implications of, let alone solutions to, such internation- al catastrophes as ozone layer depletion, global warming and species extinction. There is nevertheless growing acceptance of the notion that arrogance, ignorance and greed, combined with overpopulation and powered by technology, are responsible for such severe resource exploitation and * LL.B. (Toronto), LL.M. (Monash). First Secretary, Australian Permanent Mission to the United Nations, New York. Former Head of the Environmental Law Unit, Legal Office, Australian Department of Foreign Affairs and Trade, Canberra.