55 results were found for H 정보이용료현금화 「TKTAKA9.COM」 티켓타카 I 정보이용료현금화 전문 포탈 구글정보이용료상품권✔소개된 가격대였습니다./.

Results:

• 51. Recent publications

  changes, bias-estimation of mass-balance measurements and changes in subglacial lakes derived by LiDAR-mapping of the surface of Icelandic glaciers. Annals of Glaciology 54(63), 63–74, 10.3189/2013AoG63A422. Viggó Þór Marteinsson, Árni Rúnarsson, Andri Stefánsson, Þorsteinn Þorsteinsson, Tómas Jóhannesson, Sveinn H. Magnússon, Eyjólfur Reynisson, Bergur Einarsson, N. Wade, H. G. Morrison & E /about-imo/arctic/completed-projects/publications/

• 52. CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction

  of climate change on the routine and periodic maintenance of roads. Helsinki 2009. Finnish Road Administration, Central Administration. Finnra reports 8/2009, 66 p. + app. 8 p. ISSN 1459-1553, ISBN 978-952-221-172-9, TIEH 3201122-v. (in Finnish, abstract in English) [5] Salanne, i., Byring, B., Valli, R., Tikkanen, R., Peltonen, P., Haapala, J., Jylhä, K., Tolonen-Kivimäki, O., and Tuomenvirta, H /media/loftslag/CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction.pdf

• 53. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 54. Kok_JGEC658_2009

  Change 19 (2009) 122–133 A R T I C L E I N F O Article history: Received 14 November 2007 Received in revised form 21 August 2008 Accepted 25 August 2008 Keywords: Fuzzy Cognitive Maps Scenario Participation Resilience Brazil A B S T R A C T The main drawback of the Story-and-Simulation approach is the weak link between qualitative and quantitative scenarios. A semi-quantitative tool, Fuzzy /media/loftslag/Kok_JGEC658_2009.pdf

• 55. 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