84 results were found for P 정보이용료현금화 〔tktaka¸com〕 티켓타카 Q 정보이용료현금화 전문 포탈 카드대납업체🦏bordello/.

Results:

• 31. Paper-Olafur-Rognvaldsson_91

  High-resolution regional climate simulations over Iceland using polar MM5. Mon. Wea. Rev., 133, 3527– 3547. Buzzi A., Tartaglione N. and Malguzzi P. 1998. Numerical simulations of the 1994 Piedmont flood: Role of orography and moist processes. Mon. Wea. Rev., 126, 2369–2383. Chiao, S., Lin Y.-L. and Kaplan M. L. 2004. Numerical study of the orographic forcing of heavy precipitation during MAP IOP /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 32. 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

• 33. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  Grin’s work on this article was part of the programme of the Dutch Knowledge network on System Innovations (KSI). P. Huntjens (&)  C. Pahl-Wostl Institute for Environmental Systems Research, University of Osnabruck, Barbarastraße 12, Geb. 66, 49069 Osnabruck, Germany e-mail: patrickhuntjens@yahoo.com J. Grin Amsterdam School for Social Science Research, University of Amsterdam, Amsterdam /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 34. ces-glacier-scaling-memo2009-01

  of melt water from glaciated areas in long integrations for a warming climate. Glacier dynamics This problem can be qualitatively analysed by considering the continuity equation for ice vol- ume, which may be expressed as ¶h ¶t + ¶q ¶x = b or ¶h ¶t +~ ~q = b ; (1) for a one-dimensional ice flow channel or an ice cap that flows in two horizontal dimensions, respectively. h is ice thickness, q or ~q /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 35. 2010_003rs

  ca ti o n s fo r th e la rg est e a rt h q u a ke s w it h in t h e S IS Z b et w ee n 1 7 0 6 a n d 2 0 0 8 d en o te d b y w h ite fil le d c ir cles. E stim a te d f a u lt p la n es o f h is to ric a l ea rt h q u a ke s a re s h o w n a s w h ite , th ick li n es ( fr o m R o th , 2 0 0 4 ). F a u lt p la n es f ro m 1 9 9 8 ( V o g fj ö rd et a l. , 2 /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 36. CES_D2.4_task1

  --------------------------------------------------------------------------- STAID = ECA&D STATION IDENTIFIER NAME =STATION NAME CN = COUNTRY CODE HGT = HEIGHT ABOVE SEA LEVEL T = TABLES AVAILABLE FOR TEMPERATURE P = TABLES AVAILABLE FOR PRECIPITATION --------------------------------------------------------------------------- STAID NAME CN LATITUDE LONGITUDE HGT 1 VAEXJOE /media/ces/CES_D2.4_task1.pdf

• 37. Water_resources_man_Veijalainen_etal

  draw-down of at least one meter by the beginning of April. In addition to Author's personal copy Climate Change Impacts on the Vuoksi Watershed in Finland 3441 Fig. 2 Schematic presentation of the new regulation scheme for Lake Pielinen. The outflow from the lake (Q) depends on the water level and time of year. The percentages give the deviation from outflow according to the natural rating curve /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 38. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  used to explicate them” (Smith 2009). 300 Public Choice (2010) 143: 293–301 References Agrawal, A. (2002). Common resources and institutional sustainability. In National Research Council, Com- mittee on the Human Dimensions of Global Change E. Ostrom, T. Dietz, N. Dolšak, P. Stern, S. Stonich, & E. Weber (Eds.), The drama of the commons (pp. 41–85). Washington: National Academies Press. Anderson /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 39. raisanen_ruosteenoja_CES_D2.2

  in Table 2.1. Some potential limitations of using the CMIP3 ensemble for probabilistic climate change forecasting should be mentioned. First, current GCMs still have a relatively coarse horizontal resolution. Within the CMIP3 ensemble, the grid spacing varies from 1.1 q latitude × 1.1q longitude to 4 q latitude × 5q longitude (for the analysis presented here, all the model results were /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 40. TietavainenHanna_CES_2010

  the observed data sets are smaller in SW than in NE • MMM overestimates precipitation, but is closer to observations in SW than NE barb2right Better observational coverage in SW SW NE p r e c i p i t a t i o n s u m ( m m ) CES Conference, Oslo 31.5.-2.6.2010 SWNE • Precipitation trends (mm / 10 yr) in 1961-2000 according to observations and model simulations (MMM) • Including the range /media/ces/TietavainenHanna_CES_2010.pdf