85 results were found for X 홈타이△ㄲr톡 gttg5△苄신봉동오전출장魁신봉동오후출장㷕신봉동외국녀출장신봉동외국인여성출장🚆periodically/.

Results:

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

  %) 14 (26%) 39 (74%) Gender Number (%) E I S N T F P J Male 100 (48%) 47 (47%) 53 (53%) 15 (15%) 85 (85%) 59 (59%) 41 (41%) 29 (29%) 71 (71%) Female 109 (52%) 66 (61%) 43 (39%) 22 (20%) 87 (80%) 43 (39%) 66 (61%) 21 (19%) 88 (81%) Climatic Change (2012) 112:233–242 237 symposia participants were not significantly different from the preferences of the U.S. general population, which was 49 /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 62. Horsens_case

  7 1 2 3 4 5 6 7 8 9 10 11 12 Month M ea n d is ch ar g e (m 3 / s) Present: Mean A2: Mean Station 280001: Upstream Bygholm Lake 0 5 10 15 20 25 30 35 1 2 3 4 5 6 7 8 9 10 11 12 Month M ax im u m d is ch ar g e (m 3 / s) Present: Max A2: Max Station 270045: Upstream Lake Nørrestrand 0 2 4 6 8 10 12 14 16 1 2 3 4 5 6 7 8 9 10 11 12 Month M ea n d is ch ar g e (m 3 / s) Present: Max A2: Max /media/loftslag/Horsens_case.pdf

• 63. VI_2015_005

  depression .. 18 9 Relative seasonal occurrence of mean sea level pressure modes........................ 20 10 Composite mean temporal tendencies of mean sea level pressure...................... 22 11 Composite mean 500 hPa geopotential height anomalies ................................ 25 12 Composite mean surface wind speed anomalies ............................................ 27 13 Composite /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 64. GA_2009_91A_4_Andreassen

  (alb: AWS) MODELLING LONG-TERM SUMMER AND WINTER BALANCES ? The authors 2009 Journal compilation ? 2009 Swedish Society for Anthropology and Geography 241 ed temperatures relative to –20°C to account for de-cay of snow albedo at temperatures below the melt-ing point, following a study by Winther (1993). Wetested both approaches, and chose to use –5°C asthe minimum for the accumulated temperature /media/ces/GA_2009_91A_4_Andreassen.pdf

• 65. Eriksson_Garvill_Nordlund_2006

  (F ð1; 905Þ ¼ 6:89, po0:01, partial Z2 ¼ 0:008), and a larger reduction in own and others’ car use compared to the increase with two SEK/l (F ð1; 880Þ ¼ 16:96, po0:001, partial Z2 ¼ 0:019 and F ð1; 879Þ ¼ 15:64, po0:001, partial Z2 ¼ 0:017 respectively). In addition, the increase with five SEK/liter was perceived as more unfair (F ð1; 904Þ ¼ 10:06, po0:01, partial Z2 ¼ 0:011) and respon- dents /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf

• 66. Lorenzoni_Pidgeon_2006

  very/somewhat worried about the greenhouse effect (of these, 43% were very worried); in 19924 the percentage had increased to 89% (of these, 62% were very worried) (INRA (Europe), 1992). In 19955 public concern was similar: 84% declared to be very/quite worried about climate change as a global environmental threat (INRA (Europe)-ECO, 1995). By 2002 another survey (EORG, 2002) suggested /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 67. VI_2020_011_en

  / Aðal- og undirtitill: Upplag: 20 An initial volcanic hazard assessment of the Vestmannaeyjar Volcanic System: Impacts of lava flow and tephra deposit on Heimaey Fjöldi síðna: 73 Framkvæmdastjóri sviðs: Jórunn Harðardóttir Höfundar: Melissa Anne Pfeffer, Sara Barsotti, Esther Hlíðar Jensen, Verkefnisstjóri: Emmanuel Pierre Pagneux, Bogi Brynjar Björnsson, Guðrún Jóhannesdóttir, Ármann /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 68. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  ra tio n n ee ds a tho rough ,indis putable ,sci entifi c as se ss m en to ff ac ts (Fr ijte rs an d Lee ntvaa r 200 3) Th e quantit y o fdat ai sno tt he onl y issu e; dat a coll ecte d mus tals o be o fa hig h qualit y an d de pendable . 2: St at ist ic al M od el s (na tur al sy ste m ): 1: Ep ist em ic O fte n n o ts o im po rta nt M od el lin g ca pa ci ty n ee de d fo r simul atin g ef fect /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 69. ces-oslo2010_proceedings

  and Jónsson, S. Importance of groundwater modelling in hydrological modelling in Iceland and implementation of the groundwater module in the hydrological model WASIM for two water sheds in Iceland .................................... 84 Einarsson, B. and Jónsson, S. The effect of climate change on runoff from two watersheds in Iceland .............................................................. 86 /media/ces/ces-oslo2010_proceedings.pdf

• 70. VI_2020_008

  .............................................................................................................. 20 3.1 Block Maxima ....................................................................................................................... 21 3.2 Peak-over-Threshold ............................................................................................................. 22 3.3 Estimation /media/vedurstofan-utgafa-2020/VI_2020_008.pdf