65 results were found for z 파주안마Ε“otam13.com’ 파주안마 파주안마 파주키스방✤파주건마.

Results:

• 31. 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

• 32. vonKorff_etal-2010

  ” The latter is in our case a policy decision represented by point z in Fig. 1. In European water management, typical policy decisions that involve participation include water management plans. Leading up to the policy decision is the participation process, represented by the space between points y and z, in which stakeholders interact with each other but also with the agency responsible /media/loftslag/vonKorff_etal-2010.pdf

• 33. ces-glacier-scaling-memo2009-01

  ) is considered as a sequence of steps corresponding to n individual glaciers of different sizes (with volumes vi and areas si for i = 1 to n), or using V (v) = Z v 0 1 g dS ds dx ; (7) where the slope of the area distribution function, dS=ds, is considered as a function of ice vol- TóJ 5 5.12.2009 Memo 0 50 100 150 200 0 5 10 15 20 25 Cumulative area (km2) Area (km 2 ) 0 5 10 15 0. 0 0. 5 1. 0 1. 5 2. 0 2. 5 /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 34. VI_2009_006_tt

  to theoretical framework. I do also want to thank him for an enjoyable time during this work, both in the office and in the field. This work was carried out as a part of the Skaftá cauldrons research project which was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja- sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com- pany), the National Energy /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 35. VI_2016_006_rs

  Such landslides fall from a comparatively high elevation, cause extensive disruption and upheaval of loose materials and soils in their way, and can travel considerable distances uphill against opposing slopes. Secondly, there are medium-sized or large, rapid debris flows that are released from com- paratively high elevations and are confined to gullies as they travel down the mountain- side, similar /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 36. Traffc-maintenance_expenditures

  Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009 ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost operating manage- ment develop- poned-, of land grants ons European tax over- level costs ment ment comprehen- build- and com- Regional De- heads 1991- 1991- sive- and ings pensation /media/loftslag/Traffc-maintenance_expenditures.pdf

• 37. IPPC-2007-ar4_syr

  (-33%) during 1970 to 2004 has been smaller than the com- bined effect of global income growth (77%) and global population growth (69%); both drivers of increasing energy-related CO2 emis- sions. The long-term trend of declining CO2 emissions per unit of en- ergy supplied reversed after 2000. {WGIII 1.3, Figure SPM.2, SPM} Differences in per capita income, per capita emissions and energy /media/loftslag/IPPC-2007-ar4_syr.pdf

• 38. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  ) of the forthcoming changes are uncertain. This uncertainty comes from three basic sources: z Scenario uncertainty: future changes in the atmospheric composition, and thus the external forcing of the climate system, depend on the magnitude of future anthropogenic emissions of greenhouse gases and other radiatively active substances such as aerosol particles and their precursor gases. z Modelling /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 39. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  & 4 Y u a n g Z h e n g D e n m a r k F o r e s t r y & L a n d s c a p e 2 1 0 A t h a n a s i o s V o t s i s F i n l a n d U r b a n & r e g i o n a l p l a n n i n g 3 3 2 E i v i n d J u n k e r N o r w a y L a w 4 3 3 M i c h a e l L a i h o F i n l a n d E u r o p e a n s t u d i e s 5 2 0 H e c to r G u i n e a B a r r i e n to s S w e d e n N a t u r a l r e s o u /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 40. Linnet_Ulfar_CES_2010

  °C/100y 1975-2000 • 2.35 °C/100y 2000- •Change in precipitation • Average increase 4.8% / 100 y • Range 3.3 – 7.2 % •Glaciers • Results from CES • 25% decrease in volume from 2000 to 2050 Temperature transformation Com parison of series 10000 12000 14000 16000 18000 20000 22000 1 9 5 0 1 9 5 2 1 9 5 4 1 9 5 6 1 9 5 8 1 9 6 0 1 9 6 2 1 9 6 4 1 9 6 6 1 9 6 8 1 9 7 0 1 9 7 2 1 9 7 4 1 9 7 6 1 9 7 8 1 /media/ces/Linnet_Ulfar_CES_2010.pdf