91 results were found for Y アイリス〈ωωω,RTЗЗ,TOP〉コード:B77〉ミップスロット༿トラットfc🤞サッカートトサイト💛マカオベネシアン╜ソマリアの国家戦㍁パワーボールピクスター∿ジョージアサッカー␇プロトライブスコア∔.adq/.

Results:

• 41. aerodrome_summaries_20140603

  14 0 1 2 3 8 12 15 0 1 2 3 8 12 16 0 1 2 4 8 12 17 0 1 2 4 8 12 18 0 1 2 4 8 12 19 0 1 2 4 8 13 20 0 1 2 4 8 13 21 0 2 3 5 9 13 22 1 2 3 5 9 13 23 1 2 3 4 9 13 MEAN 1 2 2 4 8 13 10 AE R OD R OM E CLIM A T OLOGICA L SUMMA R Y - T ABL E D AE R OD R OME :BIK F - KEFL A VÍ K /K efl avi k PERIO D O F RECORD :2001–201 0 L A TITUDE :6 3 59’06" N LONGITUDE :2 2 36’20" W ELE V A TIO N AB O V E MSL :5 2 /media/vedur/aerodrome_summaries_20140603.pdf

• 42. Mid-Latitudes-Agenda1_nov2013EH

  polarity reversal from winter to summer in 2010 and its relation to extreme hot summer associated with polar jet, summer AO and blocking - Y Tachibana Group Discussion 10:30 – 11:00 Coffee Break 11:00 – 12:00 11:00 – 11:20 11:20 – 11:40 11:40 – 12:00 12:00 – 12:30 Potential Arctic / Mid-Latitude Linkages – Large Scale (Chair: Jim Overland) Large scale linkages between fall /media/loftslag/Mid-Latitudes-Agenda1_nov2013EH.pdf

• 43. CES_D2.4_task2_CMIP3_winds

  % 6,0 % 8,0 % 10,0 % 1 3 5 7 9 11 13 15 17 19 21 23 25 27 29 31 33 35 Fr eq ue nc y (% ) Geostrophic wind (m/s) September-April 1971-2000 2046-2065 -0,5 % -0,4 % -0,3 % -0,2 % -0,1 % 0,0 % 0,1 % 0,2 % 0,3 % 0,4 % 0,5 % 0,6 % 1 3 5 7 9 11 13 15 17 19 21 23 25 27 29 31 33 35 C ha ng e in % Wind class in m/s September-April change 46-71 Fig. 6. Top: 10-GCM mean frequency distributions of daily /media/ces/CES_D2.4_task2_CMIP3_winds.pdf

• 44. Kurpniece_Liga_CES_2010

  and corrected data -5 0 5 10 15 1 . 0 1 . 5 2 . 0 2 . 5 3 . 0 3 . 5 Temperature,°C P r e c i p i t a t i o n , m m / d a y Jan Feb Mar Apr May Jun JulAug Sep OctNov Dec Year obs ALUKSNE DMI 1961-1990 ALUKSNE mod DMI 1961-1990 ALUKSNE JanFeb Mar Apr May Jun Jul AugSep Oct Nov Dec Year Jan Feb ar Apr May Jun Jul Aug Sep Nov Dec ear After the correction all 3 climate models agree with observed data /media/ces/Kurpniece_Liga_CES_2010.pdf

• 45. Eriksson_2-Acceptability-of-policy

  for behavioural responses to policy • Psychological models of behaviour change (e.g., TPB) Ajzen & Fishbein (1991) Subjective norm Specific attitudes Perceived behavioural control Intention Behaviour Normative beliefs Behavioural beliefs Control beliefs P O L I C Y (3) Factors important for behavioural responses to policy cont. • Cost-minimization principle (Loukopoulos et al. 2006) • Barriers /media/loftslag/Eriksson_2-Acceptability-of-policy.pdf

• 46. ces-glacier-scaling-memo2009-01

  is first derived (Figure 3, left). The cumulative area distribution function S(s) (shown on the x-axis) represents total area of all glaciers with area less than s (shown on the y-axis of the figure). Typically, the total glaciated area and an estimate of the area of a few of the TóJ 4 5.12.2009 Memo a71 a71a71 a71 Area (km2) Volume (km 3 ) 10 103 105 107 1 10 2 10 4 10 6 Icelandic ice caps, v /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 47. PhD_course-Programme_26Aug2011-final

  Journal of Social Issues, 56, 407-424. Von Korff Y, d'Aquino P, Daniell KA, Bijlsma R (2010) Designing participation processes for water management and beyond. Ecology and Society 15(3): 1. http://www.ecologyandsociety.org/vol15/iss3/art1/ Samuelson CD (1993). A multiattribute evaluation approach to structural change in resource dilemmas. Organizational Behavior and Human Decision Processes /media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf

• 48. 2013_001_Nawri_et_al

  the validity of the ideal gas law, hydrostatic balance, a piecewise linear vertical gradient of air temperature, and neglecting the effects of water vapour. Pressure, p, as a function of height can then be derived through vertical integration of the hydrostatic balance equation, and is given by p(h(x;y);z) = p0 exp g R Z h(x;y)+z 0 dx T (x ) ; (5) where p0 is pressure at mean sea level, T /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 49. glacier_mass_balance_poster

  750-1170 AAR of the warm year of 2004 - digitized using the October 2004 SPOT 5 HRS images Ice cap E: Eyjafjallajökull To: Torfajökull Ti: Tindfjallajökull AAR (%) 20-25 <5 0 Method References Berthier E., Arnaud Y., Baratoux D., Vincent C. and Rémy F. 2004. Recent rapid thinning of the "Mer de Glace" glacier derived from satellite optical images. Geophys. Res. Lett., 31, L17401, doi:10.1029 /media/ces/glacier_mass_balance_poster.pdf

• 50. VI_2022_006_extreme

  and the y-axis the dates between March and July. For every year, the melt season starting date is plotted (blue dots), and a blue line connects the dates for all the years. A regression line fitting those values (orange line) is shown, and the difference in days between the beginning and the end of the period, as calculated from the regression line, is indicated at the top of the plot. In 9 cases /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf