17 results were found for WA 0821 7.

Results:

• 1. Milly_etal-2008-Stationarity-dead-Science

  This increases precipitation, and possibly flood risk, where prevailing atmo- spheric water-vapor fluxes converge (6). Rising sea level induces gradually height- ened risk of contamination of coastal fresh- water supplies. Glacial meltwater temporar- ily enhances water availability, but glacier and snow-pack losses diminish natural sea- sonal and interannual storage (7). Anthropogenic climate warming /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 2. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  & implementation 6. Information management & sharing 7. Finances and cost recovery 8. Risk management 9. Effectiveness of (international) regulation As a useful starting point for operationalization, we considered the River Basin Assessment framework devel- oped by Raadgever et al. (2008). Raadgever et al. devel- oped a framework including four regime elements (4–7). Based on relevant literature (see /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 3. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

  their audience. Climatic Change (2012) 112:233–242 DOI 10.1007/s10584-011-0205-7 C. S. Weiler (*) Office for Earth System Studies, Whitman College, Walla Walla, WA 99362, USA e-mail: weiler@whitman.edu J. K. Keller School of Earth and Environmental Sciences, Chapman University, Orange, CA 92866, USA C. Olex The Point, 121 Jewett Street, Newton, MA 02458, USA 1 Introduction Of all the applications /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 4. IPPC-2007-ar4_syr

  Arctic sea ice extent has shrunk by 2.7 [2.1 to 3.3]% per decade, with larger decreases in summer of 7.4 [5.0 to 9.8]% per decade. Mountain glaciers and snow cover on average have declined in both hemispheres. The maximum areal extent of sea- sonally frozen ground has decreased by about 7% in the Northern Hemisphere since 1900, with decreases in spring of up to 15%. Temperatures at the top /media/loftslag/IPPC-2007-ar4_syr.pdf

• 5. 2010_017

  ............................................................................................................................... 5 TABLES ................................................................................................................................. 6 1 ABSTRACT ..................................................................................................................... 7 2 INTRODUCTION /media/ces/2010_017.pdf

• 6. VI_2021_008

  Tremv-ALERT: A new early warning system to detect volcanic tremor Bethany Vanderhoof Þórður Karlsson Yesim Cubuk Sabuncu Kristín Jónsdóttir VÍ 2021-008 Skýrsla Tremv-ALERT: A new early warning system to detect volcanic tremor VÍ 2021-008 ISSN 1670- 8261 Skýrsla + 354 522 60 00 vedur @vedur . is Veður st of a Íslands Búst aðaveg ur 7 – 9 108 Reyk j avík Bethany Vanderhoof Þórður Karlsson Yesim /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 7. Journal_of_Hydrology_Veijalainen_etal

  in Finland Noora Veijalainen a,*, Eliisa Lotsari b, Petteri Alho b, Bertel Vehviläinen a, Jukka Käyhkö b a Freshwater Centre, Finnish Environment Institute, Mechelininkatu 34a, P.O. Box 140, FI-00251, Helsinki, Finland b Department of Geography, FI-20014 University of Turku, Turku, Finland a r t i c l e i n f o Article history: Received 7 January 2010 Received in revised form 13 June 2010 Accepted /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 8. Hare-2011-ParticipatoryModelling

  Dispatch: 02.08.11 CE: E E T 5 9 0 No. of Pages: 19 ME: 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 Another possible driving force behind its popularity is changing legislation requiring environmental managers and policy-makers to increase stakeholder participation in their work [e.g /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 9. VI_2009_006_tt

  during the Holocene . . . . . . . . . . . . . . 6 2.5 Jökulhlaups in America and Asia at the end of the last glaciation . . . 7 2.6 Jökulhlaup sediment concentration and Lahars . . . . . . . . . . . . . 8 3 The Skaftá cauldrons and jökulhlaups in Skaftá 9 3.1 The subglacial lakes . . . . . . . . . . . . . . . . . . . . . . . . . . . 9 3.2 Jökulhlaups in Skaftá /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 10. Observations - Árnes

  GMT -0.1° NE 7 Max wind : 8 / 11 07 GMT -1.2° NE 6 Max wind : 6 / 10 06 GMT -1.5° NE 6 Max wind : 7 / 10 05 GMT -2.3° ENE 6 Max wind : 6 / 10 04 GMT -3.1° NE 6 Max wind : 7 / 10 03 GMT -2.2° NNE 7 Max wind : 7 / 10 02 GMT -1.9° NNE 7 Max wind : 7 / 11 01 GMT -2.2° NE 4 Max wind : 5 / 9 00 GMT -2.1° NE 3 Max wind : 7 / 10 /m/observations/areas