79 results were found for V 신용카드현금화 【TKTAKA1༝COM】 티켓타카 W 신용카드현금화 전문 포탈 문상현금화👩🏿‍💻concession/.

Results:

• 61. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  was used as a reference map for co-registration and correction of the vertical offset of the other DEMs. The average specific mass balance was estimated from the mean elevation difference between glaciated areas of the DEMs. The glacier mass balance declined significantly between the two periods: from 0.2 to 0.2 m yr1 w. eq. during the earlier period (1980s through 1998) to 1.8 to 1.5 m yr1 w /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 62. Kok_1-scenarios-lecture-1

  : to use or not to use? *O'Neill, R. V., and A. W. King. 1998, Homage to St. Michael; or, why are there so many books on scale?: Pages 3–15 in D. L. Peterson and V. T. Parker (editors). Ecological scale: theory and applications. Columbia University Press, New York. • Robert O’Neill questions the unifying capabilities* • Aspects of the land use system have different scale properties • To use /media/loftslag/Kok_1-scenarios-lecture-1.pdf

• 63. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  improving management policies and practices by learning from the outcomes of implemented management strategies. Partici- patory integrated assessment is here a form of problem structuring for identification of gaps, ambiguity and multiple frames, confrontation, and integration of the most divergent views with respect to a given problem situation. Additional methods and tools that AM require com /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 64. Kok_JGEC658_2009

  to be simple and therefore has important drawbacks. Future improvements should be made in the light of applications within a larger toolbox of scenario methods.  2008 Elsevier Ltd. All rights reserved. * Tel.: +31 317 482422; fax: +31 317 419000. E-mail address: kasper.kok@wur.nl. Contents lists available at ScienceDirect Global Environmental Change journa l homepage: www.e lsev ier .com/ locate /media/loftslag/Kok_JGEC658_2009.pdf

• 65. Milly_etal-2008-Stationarity-dead-Science

  A. Dunne, A. V. Vecchia, Nature 438, 347 (2005). 16. J. C. Knox, Quatern. Sci. Rev. 19, 439 (2000). 17. P. C. D. Milly, R. T. Wetherald, K. A. Dunne, T. L. Delworth, Nature 415, 514 (2002). 18. Z. W. Kundzewicz et al., Hydrol. Sci. J. 50, 797 (2005). 19. R. Seager et al., Science 316, 1181 (2007). 20. IPCC, in Climate Change 2007: Mitigation of Climate Change, Contribution of WG3 to AR4, B /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 66. VI_2015_006

  Differences in net shortwave flux due to differences in cloud cover (compare with Figure 5) are especially noticeable on 27 July and 3 August around (local) noon when, off the south and southwest coast, the net flux under clear skies is increased by up to 300 W m 2, compared with neighbouring cloud-covered regions. Although, generally, there was a more extensive cloud cover over the land on 3 August than /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 67. Kok_and_Veldkamp_editorial_ES-2011-4160

  2004. Further towards a taxonomy of agent-based simulation models in environmental management. Mathematics and Computers in Simulation 64(1):25-40. Henle, K., W. Kunin, O. Schweiger, D. S. Schmeller, V. Grobelnik, Y. Matsinos, J. Pantis, L. Penev, S. G. Potts, I. Ring, J. Similä, J. Tzanopoulos, S. van den Hove, M. Baguette, J. Clobert, L. Excoffier, E. Framstad, M. Grodzinska-Jurczak, S. Lengyel, P /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 68. Sea ice in June 2010

  an ice strip at 66°42'N and 24°15' W up to 66°59'N and 22°24'W. On the 14th an observation was also received from the weather station „Hraun á Skaga“ on an iceberg 10-11 nm northwest of Skagatá. On the 22nd an ice strip was observed at 66°49'N and 22°22'W until 66°51'N and 22°09'W. On the 29th two icebergs were observed in Þverál. IMO issued information and an image of the ice edge 16th June. Wind /sea-ice/monthly/2010/nr/2341

• 69. Sea ice in May 2010

  An ice edge was observed in the area from 67°31'N and 023°35'W to 66°41'N and 23°43'W. Westerlies were a little more prevailing in the Greenland Strait and north of Iceland than on average /sea-ice/monthly/2010/nr/2340

• 70. Sea ice in August 2010

  reported on a floe on 66°12,67'N 27°38,17'W and on the 30th a ship observed a large iceberg in location 66°56'N 24°44,4'W. Wind directions were close to the average on the Greenland Strait this month /sea-ice/monthly/2010/nr/2343