32 results were found for 도쿄카지노〔TRRT2‸COM〕 도쿄바카라 도쿄포커◈도쿄바둑이❸도쿄슬롯 NSN/.

Results:

• 21. 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

• 22. VI_2015_009

  M A M J J A l ll l l l l l l l lll l l lll 0 100 200 300 60 0 80 0 100 0 Days since Sept. 1st Q (m ³/s ) vhm102 S O N D J F M A M J J A l l l ll l l l l l l l l l l l l l ll l l l l l l 0 100 200 300 30 40 50 60 70 Days since Sept. 1st Q (m ³/s ) vhm116 S O N D J F M A M J J A l l l l l l l l l l l l l l l l l l l l l l l l l l 0 100 200 300 20 0 30 0 40 0 50 0 Days since Sept. 1st Q (m ³/s /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 23. Hare-2011-ParticipatoryModelling

  ; mayo ran d governmen t of cer s F M (si m u lat ion m od el) M F Tabl e2 . Ca te go riz at io n ta bl e fo r th e ex am pl es o fF AB E ap pr o ac he s to pa rt ic ip at o ry m o de llin g. A ce ll in th e ‘ pa rt ic ip at o ry m o de llin g st ag e’ ca n be interprete d in th e fo llo w in g m an n er : w he re th er e is n o st ak eh o ld er in vo lve m en t, N O P is w rit te n . W he re th /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 24. Kok_JGEC658_2009

  it will be one of the main aspects of this paper. 2.3. Properties The elements of a Fuzzy Cognitive Map are as follows:  Concepts: C1, C2, . . ., Cn. These represent the drivers and constraints that are considered of importance to the issue under consideration.  State vector: A = (a1, a2, . . ., an), where ai denotes the state of the node Ci. The state vector represents the value of the concepts /media/loftslag/Kok_JGEC658_2009.pdf

• 25. Lorenzoni_Pidgeon_2006

  : PidgeonN@cardiff.ac.uk Climatic Change (2006) 77: 73–95 DOI: 10.1007/s10584-006-9072-z c© Springer 2006 74 I. LORENZONI AND N. F. PIDGEON national policies strongly on fossil fuels. The British Prime Minister encapsulated these tensions when he recently stated that there is “no bigger long-term question facing the global community” than climate change (BBC, 2004), whilst emphasising the need /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 26. Reykholt-abstracts

  Lidar measurements of the cryosphere Reykholt, Iceland, June 20–21, 2013 Lidar measurements of the cryosphere Reykholt, Iceland, June 20–21, 2013 Abstract volume Lidar map of the ice-covered stratovolcano Öræfajökull in S-Vatnajökull, S-Iceland, surveyed by TopScan GmbH in August 2011 Lidar measurements of the cryosphere /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 27. VI_2016_006_rs

  wide and 1000 m long shelf called Þófi, terminating at 80–100 m a.s.l., see Map 4. The inclination of the shelf is 15 on average. The surface of Þófi is covered with unconsolidated glacial till and landslide deposits and marked with five gullies. The brook called Þófalækur near the middle of the shelf divides it into an inner and outer part. On the outermost part of the shelf, there is a small /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 28. VI_2019_009

  the automatic station shows 0 the manual station shows 15 (precipitation is more than 5 km distance) in 20 cases. In 22 cases the manual station shows 21 62 (Rain, not freezing, intermittent, moderate at time of observation) while the automatic station shows 61 (light rain). 0 250 500 750 1000 0 1 2 3 10 11 15 16 20 21 23 24 25 26 40 41 50 51 52 53 58 60 61 62 63 64 67 70 71 72 73 80 81 83 84 85 Present /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 29. 2013_001_Nawri_et_al

  the Fljótsdalsheiði region . . . . . . . 47 18 Seasonal mean wind power density within the Fljótsdalsheiði region . . . . . . . . 48 19 Directional mean wind power density within the Gufuskálar region . . . . . . . . . 49 20 Seasonal mean wind power density within the Gufuskálar region . . . . . . . . . . 50 21 Directional mean wind power density within the Hellisheiði region . . . . . . . . . 51 22 Seasonal mean /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 30. VI_2020_004

  ........................................................................................ 94 6.1 Tephra fallout impact during an eruption at Hekla, like 1980 ................................... 94 6.2 Tephra fallout impact during an eruption at Katla, like 1918 .................................... 94 6.3 Tephra fallout impact during an eruption at Öræfajökull, like 1362 ......................... 95 6.4 Recommendations and next steps /media/vedurstofan-utgafa-2020/VI_2020_004.pdf