80 results were found for p 보성2부ｗ［zzan1.com〕▲보성텐 보성가요주점♗보성요정 보성한잔해.

Results:

• 21. program17012012

  Airborne Measurements of Volcanic Ash - results from Eyja and the new Met Office Civil Contingency Aircraft Jonathan P. Taylor, UK Met Office 11:15 Observational systems for monitoring of volcanic ash Sibylle von Löwis, Geirfinnur S. Sigurðarson, IMO 11:45 NAME dispersion model, an introduction Jonathan P. Taylor, UK Met Office 12:15 – 13:30 Lunch break The volcanic ash problem /media/vedurstofan/utgafa/hlidarefni/program17012012.pdf

• 22. IPPC-2007-ar4_syr

  (-33%) during 1970 to 2004 has been smaller than the com- bined effect of global income growth (77%) and global population growth (69%); both drivers of increasing energy-related CO2 emis- sions. The long-term trend of declining CO2 emissions per unit of en- ergy supplied reversed after 2000. {WGIII 1.3, Figure SPM.2, SPM} Differences in per capita income, per capita emissions and energy /media/loftslag/IPPC-2007-ar4_syr.pdf

• 23. Group-1_Scenarios-for-AWM

  i on c a p ac i t y A r ea of r e s i d en c e (Flood p r one /non p r one a r eas) Un c e r t a n t i e s H i g h wi l l i n g n e s s t o p a y L o w wi l l i n g nes to pay D i k e s H i gh t a x a t i on - E arly w arn i n g s y s t e m s - Sof t s t r uct u r a l m e as u r e s -Community training L o w taxation Risk P e r c e p t i o n B e n e f i /media/loftslag/Group-1_Scenarios-for-AWM.pdf

• 24. Refsgaard_etal-2007-Uncertainty-EMS

  Refsgaard a,*, Jeroen P. v Peter A. Vanroll a Geological Survey of Denmark and Greenlan b Copernicus Institute for Sustainable Development and Innovation Utrecht University, Utrecht c Environmental Modelling & Softwar equitable manner without compromising the sustainability of * Corresponding author. Tel.: þ45 38 142 776; fax: þ45 38 142 050. E-mail address: jcr@geus.dk (J.C. Refsgaard). 1364-8152 /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 25. Protective measures

  developments (European Commission, Directorate-General for Research, Publication EUR 23339, 2009, ISBN 978-92-79-08885-8, ISSN 1018-5593, DOI 10.2777/12871. Edited by T. Jóhannesson, P. Gauer, P. Issler and K. Lied. Contributions by M. Barbolini, U. Domaas, T. Faug, P. Gauer, K. M. Hákonardóttir, C. B. Harbitz, D. Issler, T. Jóhannesson, K. Lied, M. Naaim, F. Naaim-Bouvet and L. Rammer) (pdf 1.6 Mb; high /avalanches/imo/protective/

• 26. The design of avalanche protection dams

  be ordered at the EU Bookshop and it can be accessed on the web both as PDF suitable for the screen (1.5 Mb) and in higher resolution suitable for printing (27.9 Mb). Edited by T. Jóhannesson of the Icelandic Meteorological Office and by P. Gauer, P. Issler and K. Lied of the Norwegian Geotechnical Institute. Contributions by M. Barbolini, U. Domaas, T. Faug, P. Gauer, K. M. Hákonardóttir, C. B /about-imo/news/nr/1631

• 27. Machguth_Horst_CES_2010

  Horst Machguth, Andreas Ahlstrøhm, GEUS, Copenhagen Surface Mass Balance of the Greenland Ice Sheet in the Paakitsoq Area, Illulisat, West Greenland - Scenarios and Related Uncertainties 2 / 16 previous work A. P. Ahlstrøm Paakitsup Akuliarusersua (Paakitsoq) Thomsen & Olesen (1990) 2 / 16 previous work Paakitsup Akuliarusersua (Paakitsoq) Thomsen (1989) Thomsen & Olesen (1991) glacial /media/ces/Machguth_Horst_CES_2010.pdf

• 28. Jens_Christian_Refsgaard_(GEUS,_Dk)

  of uncertainty (statistical uncertainty, scenario uncertainty, qualitative uncertainty, recognised ignorance and total ignorance) as well as the nature of uncertainy (epistemic and onthological uncertainty). Finally, the presentation will briefly introduce different types of methodologies for uncertainty characterisation and assessment. References: Walker WE, Harremoës P, Rotmans J, Van der Sluijs /media/loftslag/Jens_Christian_Refsgaard_(GEUS,_Dk).pdf

• 29. Adalgeirsdottir-etal-tc-5-961-2011

  were carried out to obtain the flow and sliding parameters for Hoffellsjökull that resulted in a good simulation of the observed 20th century evolution of the glacier geometry. The obtained values for the rate factor and the sliding parameter are A= 4.6× 10−15 s−1 kPa−3 and C = 10× 10−15 m a−1 Pa−3, respectively. The ice divide is kept at a fixed location in the model com- putations presented here /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 30. VI_2015_005

  model grid point must be taken into account. At latitude f , the grid-box size is given by dA = a2 cosf dldf ; (1) where a = 6371 km is the Earth’s mean radius, and latitude and longitude are measured in radians. For the ECMWF reanalyses, angular grid-point spacing dl = df = p=180 is constant across the domain. The low-pressure centre count at each grid point is then multiplied by dA=dA, with mean /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf