82 results were found for k 동대문타이Ｄ〈dm080.com”✰동대문안마※동대문주점 동대문오피 동대문주점.

Results:

• 1. 2010_005_

  which are significantly lower com- pared with similar beginning and end years. Consequently, for the 2004–50 period, the average RCM warming rates of 0.29 K per decade over the ocean, and 0.35 K per decade over the land are somewhat larger than for the reduced IPCC ensemble mean. Additionally, the tabulated values of SAT differences between the 1961–90 control period and either the 2021–50 /media/ces/2010_005_.pdf

• 2. Laboratory experiments

  of snow avalanches agains dams and retarding obstacles: A laboratory study of the interaction between supercritical, shallow flows and dams (IMO Int. Rep. 03038, 2003, authors K. M. Hákonardóttir, A. Hogg and T. Jóhannesson) (pdf 1.3 Mb) Avalanche braking mound experiments with snow. Switzerland − March 2002 (IMO Int. Rep. 03023, 2003, authors K. M. Hákonardóttir, T. Jóhannesson, F /avalanches/imo/lab/

• 3. Hazard zoning

  : Estimation of avalanche risk (IMO Rep. VÍ-R99001-ÚR01, authors K. Jónasson S. Þ. Sigurðsson and Th. Arnalds) (pdf 0.5 Mb) Avalanche hazard zoning in Iceland based on individual risk (Annals of Glaciology, 38, 285−290, 2004, authors Th. Arnalds, K. Jónasson and S. Þ. Sigurðsson) (pdf 0.4 Mb) A map on a selected front page shows recent observations of avalanches. For user access /avalanches/imo/hazard/

• 4. AnneFleig_May2010_CES

  Regional hydrological droughts in north-western Europe and associated weather types Anne K. Fleig (1), Lena M. Tallaksen (1), Hege Hisdal (2) & David M. Hannah (3) (1) University of Oslo, (2) Norwegian Water Resources and Energy Directorate, (3) University of Birmingham. CES conference, Oslo, Norway, 31 May - 2 June 2010 Bewl Reservoir in southeast England, February 2006. (Photo: Reuters /media/ces/AnneFleig_May2010_CES.pdf

• 5. Group5-Stakeholders_involvement

  - m a k e r P u b l i c S t ron g Go v ernanc e I n s u re r s Pri v a t e S t ron g M ar k e t S c ie n t i f i c e x per t s ( g eo s c ie n c e s , e c o n o m i c s , s o c iolog y , p s y c hol o g y ) Publi c / pri v a t e - - I nd u s t ri e s Pri v a t e S t ron g M ar k e t W a t e r s upplie r P u b l i c S t ron g M ar k e t F ar m er s /media/loftslag/Group5-Stakeholders_involvement.pdf

• 6. norsem_slunga

  an Hoek (1978) published a very often referenced picture showing observed crustal stresses by plotting the depth against the ratio between the mean horizontal stress and the vertikal stress. This ratio is often denoted k and thus k = (SH+Sh)/2/Sv. The main feature of the data set was the clear excess of horizontal stresses at very shallow depths, especially above some 300m. A large number /media/norsem/norsem_slunga.pdf

• 7. VI_2014_005

  of the Westfjords. Assuming a standard ver- tical temperature lapse rate of 6.5 K km 1, these differences in terrain elevation alone may be responsible for absolute differences of up to 2 K between longterm averages of simulated and measured surface air temperatures, possibly with opposite signs at nearby locations. As shown in Figure 3 (b), differences in terrain elevation are reduced if the model /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 8. 2005EO260001

  up to ~13 km height. BY K. S. VOGFJÖRD, S. S. JAKOBSDÓTTIR, G. B. GUDMUNDSSON, M. J. ROBERTS, K. ÁGÚSTSSON, T. ARASON, H. GEIRSSON, S. KARLSDÓTTIR, S. HJALTADÓTTIR, U. ÓLAFSDÓTTIR, B. THORBJARNARDÓTTIR, T. SKAFTADÓTTIR, E. STURKELL, E. B. JÓNASDÓTTIR, G. HAFSTEINSSON, H. SVEINBJÖRNSSON, R. STEFÁNSSON, AND T. V. JÓNSSON Research, 2005), which are complemented by three continuous GPS stations /media/jar/myndsafn/2005EO260001.pdf

• 9. 2013_001_Nawri_et_al

  rather than from the data directly. This reduces the amount of data that needs to be disseminated to a few parameters, that describe each wind speed distribution. Of the various probability density functions for boundary-layer wind speeds, s, the 2-parameter Weibull distribution, f (s;A;k) = k A s A k 1 exp s A k ; (1) is the one most commonly employed for wind energy studies (Morgan /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 10. Protective measures

  to avalances: An overview of the need for avalanche protection measures in Iceland (IMO Rep. 96004, 1996, authors T. Jóhannesson, K. Lied, S. Margreth and F. Sandersen) [summary of IMO publication 96003/96004] (html) Adaptation of the Swiss Guidelines for supporting structures for Icelandic conditions (IMO Int. Rep. 99013, 1999, authors T. Jóhannesson and S. Margreth) (pdf 0.1 Mb) Addendum /avalanches/imo/protective/