Search

91 results were found for y 광안리아로마ㅒ《dm080.com」✺광안리안마♦광안리업소✆광안리유흥✄광안리키스방.


Results:

  • 41. vonKorff_etal-2010

    Copyright © 2010 by the author(s). Published here under license by the Resilience Alliance. Von Korff, Y., P. d'Aquino, K. A. Daniell, and R. Bijlsma. 2010. Designing participation processes for water management and beyond. Ecology and Society 15(3): 1. [online] URL: http://www. ecologyandsociety.org/vol15/iss3/art1/ Synthesis, part of a Special Feature on Implementing Participatory Water /media/loftslag/vonKorff_etal-2010.pdf
  • 42. Refsgaard_2-uncertainty

    - nitrate reduction in underground medium medium large large large Model technical uncertainty - numerical approximation small small medium small - bugs in software medium medium small SUM: Importance Type of uncertainty Error propagation Box 1 Error propagation rules using standard deviation (σ ) Addition and Subtraction: z = x + y + .. or z = x - y - .. ..)()( 22 ++= yxz σσσ /media/loftslag/Refsgaard_2-uncertainty.pdf
  • 43. 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
  • 44. 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
  • 45. 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
  • 46. 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
  • 47. 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
  • 48. 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
  • 49. 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
  • 50. VI_2014_006

    the com- plexity of the hydrological processes through modelling, but its application is usually limited to the short-range. Although the results demonstrated a great potential for this method, its success- ful application in real-time will strongly depend on the quality and availability of streamflow observations, which can be poor or simply missing during periods of variable durations, e.g /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

Page 5 of 10






Other related web sites


This website is built with Eplica CMS