72 results were found for m 금정주점╃「dm080.com〕♦금정건마✻금정안마♡금정타이✳금정안마.

Results:

• 1. Veðurstöðvar

  Akureyri (sk) O F M I Akureyri - Krossanesbraut (sj) I Arnarnesvegur (sj) O F M I Austurárdalsháls (sj) O I Árnes (sj) O F M I Ásbyrgi (sj) O F M I Ásgarður (sj) F M I Ásgarður (sk) O I Bakkagerði (sj) O I Básar á Goðalandi (sj) O I Biskupsháls (sj) O I Bíldudalur (sj) O F M I Bjargtangar (sj) O F M I Bjarnarey (sj) O F M I Bjarnarfjarðarháls (sj) I Björg í Kinn (sj) O I Bláfeldur (sj) O F M I /weather/stations/

• 2. GA_2009_91A_4_Andreassen

  MODELLING LONG-TERM SUMMER AND WINTER BALANCES AND THE CLIMATE SENSITIVITY OF STORBREEN, ? The authors 2009 Journal compilation ? 2009 Swedish Society for Anthropology and Geography 233 MODELLING LONG-TERM SUMMER AND WINTER BALANCES AND THE CLIMATE SENSITIVITY OF STORBREEN, NORWAY BYLISS M. ANDREASSEN1,2 AND JOHANNES OERLEMANS3 1Section for Glaciers, Snow and Ice, Norwegian Water Resources /media/ces/GA_2009_91A_4_Andreassen.pdf

• 3. VI_2015_009

  between November and May, whereas for vhm102, vhm162 and vhm233, which are primarily of glacial origin, the AMF is mainly occur- ring between June and September. 7 2.3 Meteorological data Gridded daily air temperature at 2 m above ground (Crochet & Jóhannesson, 2011) and precip- itation (Crochet, 2013) calculated on a 1x1 km grid for the period 1961–2014, were used in the study. 2.4 Other data /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 4. Linnet_Ulfar_CES_2010

  2015, 2025, 2035 and 2050 North (Blanda) East (Karahnjukar) South (Thorisvatn) Change in average inflow to the main storage reservoirs Watershed A v e r a g e i n f l o w [ m 3 / s ] 0 2 0 4 0 6 0 8 0 1 0 0 1 2 0 Last 50 years Last 20 years Last 15 years Last 10 years Last 5 years Temperature corrected Transformation of climate measurements •Change in temperature • 0.75 °C/100y 1950-1975 • 1.55 /media/ces/Linnet_Ulfar_CES_2010.pdf

• 5. Hare-2011-ParticipatoryModelling

  support ) Improv e mode l (integration) ; socia llea rnin g Farmers ,loca l aut horities , association s NO P IN D Cognitiv e mappin g HE T GM B NO P HE T Simulation - by-han d OT :Researcher s KA F F Iska r (Phas e1 ) Co n ce pt u al m o de l (D is cu ss io n su pp o rt ; Com m unication ) Improv e mode l (integration) ; socia llea rnin g Nationa l poli cy-maker s NO P IN D Cognitiv e mappin g HE /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 6. VI_2013_008

  combinations indicate the type of river, with the first letter indicating the primary type. Direct runoff river (D), presence of lakes (S), glacier-fed river (J), groundwater (L). Gauging station vhm vhm vhm vhm vhm vhm 19 10 26 145 66 64 Name Dynjandisá Svartá Sandá Vestari- Hvítá Ölfusá Jökulsá Type of river D+L D+L D+L D+J+L L+J L+D+J+S Drainage area (km 2) 42 397 267 850 1664 5687 Mean altitude (m a.s.l /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 7. IMO_AnnualReport2014

  of events closely. Photo: Sigurlaug Gunnlaugsdóttir. Bárðarbunga Pálmi Erlendsson, Bergur H. Bergsson and others installing GPS and com- munication equipment. Photos: Þorgils Ingvarsson and Benedikt G. Ófeigsson. I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4 5 The magma intrusion from Bárðarbunga to the eruption site at Holuhraun and related tremor pulses /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 8. Adalgeirsdottir-etal-tc-5-961-2011

  were carried out to obtain the flow and sliding parameters for Hoffellsjökull that resulted in a good simulation of the observed 20th century evolution of the glacier geometry. The obtained values for the rate factor and the sliding parameter are A= 4.6× 10−15 s−1 kPa−3 and C = 10× 10−15 m a−1 Pa−3, respectively. The ice divide is kept at a fixed location in the model com- putations presented here /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 9. Journal_of_Hydrology_Veijalainen_etal

  24 July 2010 This manuscript was handled by K. Georgakakos, Editor-in-Chief, with the assistance of Ercan Kahya, Associate Editor Keywords: Climate change Flood Hydrological modelling Flood inundation area Hydraulic modelling Finland s u m m a r y This paper provides a general overview of changes in flooding caused by climate change in Finland for the periods 2010–2039 and 2070–2099. Changes /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 10. vanRoosmalen_etal-2009-WRR_2007WR006760

  impacts were simulated using climate-forcing data for the SRES A2 and B2 scenarios [IPCC, 2000] for the period 2071–2100 and by raising the sea level to +0.5 m above sea level (masl) and +1 masl. The land use change effects include impacts on irrigation de- mand, doubling the area with forest at the expense of grain and grass, changes in crop development dates, and a reduction in crop /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf