84 results were found for WA 0821 7001 0763 (FORTRESS) motif pintu besi minimalis Ma U Kabupaten Nias Sumatera Utara.

Results:

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

  theory to applications. Dedham, MA: Artech House. Wise S.M. 2000. Assessing the quality for hydrological applications of digital elevation models derived from con- tours. Hydrological Processes 14, 1909
  1929. Zwally H.J., Schutz B.E., Abdalati W., Abshire J., Bentley C., Brenner A., Bufton J., Dezio J., Hancock D., Harding H., Herring T., Minster B., Quinn K., Palm S., Spinhirne J. & Thomas R. 2002 /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 72. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 73. VI_2015_005

  /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 74. Water_resources_man_Veijalainen_etal

  /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 75. VI_2020_008

  − �1 + ���� � ���� − ���� ���� �� −1 ����⁄ where x is the threshold excess, u is the threshold, σ the scale parameter and ξ the shape parameter. Note that ξ is equal to the shape parameter of the corresponding GEV distribution. Return level r is defined as the value that is exceeded once every m observations and can be calculated as follows: ���� = � ���� + ���� ���� �(������������) ���� − 1 /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 76. VI_2022_006_extreme

  J. Roberts Tinna Þórarinsdóttir VÍ 2022-006 Skýrsla +3 5 4 522 6000 vedur@ve d u r.i s Veðursto f a Ísland s B ú sta ð a rve g u r 7–9 108 Reyk j a vík Contents 1 INTRODUCTION .................................................................................................................. 4 2 STUDY AREA /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 77. VI_2014_006

  and candidate situations is evaluated with the Teweles-Wobus (S1) skill score (Wilks, 1995). The S1 score compares the shape of two fields by considering their gradient at each grid point of the analogy domain: S1(u) = 100 n 1 i=1 m j=1 jDAi DFij+ n i=1 m 1 j=1 jDA j DFjj n 1i=1 m j=1 Gi + n i=1 m 1 j=1 G j (3) with DAi = A(i+1; j;u) A(i; j;u) (4) DFi = F(i+1; j; t) F(i; j; t) (5) DA j /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 78. Refsgaard_etal-2007-Uncertainty-EMS

  Discrete numerical Categorical Narrative Constant in space and time A1 A2 A3 4Varies in time, not in space B1 B2 B3 Varies in space, not in time C1 C2 C3 It is noticed that the matrix is in reality three-dimensional (source, type, nature). Thus, the categories type and nature are not mutually exclusive, and it may be argued that the ma- trix should be modified in such a way that the two uncer /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 79. Publications

  of glaciers to climate change - case studies on Storglaciären and Hofsjökull. Presented at the European Conference on Impacts of Climate Change on Renewable Energy Sources, Reykjavik, Iceland, June 5-9. [Extended abstract] Hock, R., Jansson, P., & Braun, L. (2005). Modelling the response of mountain glacier discharge to climate warming. In U. M. Huber, H. K. M. Bugmann & M. A. Reasoner (Eds.), Global /climatology/research/ce/publications/

• 80. GA_2009_91A_4_Andreassen

  /media/ces/GA_2009_91A_4_Andreassen.pdf