39 results were found for 【H-PAY.ORG】B站官方账号大全 35iao.

Results:

• 21. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

  = {0, . . . ,20}. The second option, option b, is such that the dictator keeps 18 points for herself and gives two points to the receiver: the distribution (18,2). In decision 1, the dictator thus chooses between the distribution (0,0) (zero for herself and zero for the receiver) and the distribution (18,2) (18 for herself and two for the receiver); in decision 2, the choice is between (1,1 /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 22. Lettenmaier_Dennis_CES_2010pdf

  Withdrawal Reliability Grand Coulee Recreation Reliability R e l i a b i l i t y ( % , m o n t h l y b a s e d ) Control Period 1 Period 2 Period 3 RCM 2040-2069 60 80 100 120 140 Firm Hydropower Annual Flow Deficit at McNary P e r c e n t o f C o n t r o l R u n C l i m a t e PCM Control Climate and Current Operations PCM Projected Climate and Current Operations PCM Projected /media/ces/Lettenmaier_Dennis_CES_2010pdf.pdf

• 23. Guidelines2-for-rapporteurs

  G u i n e a B a r r i e n to s P a t r i c k D r i s c o l l A n j a W e j s T o mm y C h a n K a r o l i i n a P i l l i - S i h v o l a J u s s i Y l h ä i s i K a r e n L u n d g r e n V ä i n ö N u r m i J i a o X i H a n s - P a u l V e l e m a p l e n a r y 1 ( o p e n i n g ) X s e s s i o n 1 . 1 X s e s s i o n 1 . 2 X s e s s i o n 1 . 3 X s e s s i o n 1 /media/loftslag/Guidelines2-for-rapporteurs.pdf

• 24. norsem_bryndis

  than 30,000 earthquakes at 5–7 km depth, advancing in short bursts at 0.3–4.7 km/h. Following each surge forward, the seismicity behind the dyke tip dropped, implying that the subsequent dyke opening was mostly aseismic. More detailed analyses of the seismic data recorded by a dense network around the Vatnajökull icecap have revealed small magnitude, long-period (LP or B-type) events which /media/norsem/norsem_bryndis.pdf

• 25. norsem_lund

  The recent Bothnian Bay M4.1 earthquake: where, how and why? B. Lund1, M. Uski2, H. Shomali1, D. Buhcheva1, S. Amini1, J. Kortström2 1Dep. of Earth Sciences, Uppsala University, Sweden 2Institute of Seismology, Dep. of Geosciences and Geography, University of Helsinki, Finland On 19 March 2016 a magnitude 4.1 earthquake occurred in the Bothnian Bay, between northern Sweden /media/norsem/norsem_lund.pdf

• 26. General about the project

  Publications and presentations General about the project Other international Björnsson, H. & Snorrason, Á. (2009 /ces/publications/nr/1936

• 27. Hydropower, Hydrology

  to climate change impact studies in hydrology. Proceedings from the Nordic Hydrological Conference - Reykjavík, Iceland, 11-13 August 2008, Vol.1, pp.256-265. Wong, W.K., Beldring, S., Haddeland, I. & Hisdal, H. (2010). Climate Change effects on droughts in Norway. Global Change: Facing Risks and Threats to Water Resources, IAHS Publ. 340, 198-204. National Einarsson, B. & Jónsson, S. (2010 /ces/publications/nr/1938

• 28. Paper-Olafur-Rognvaldsson_91

  Pálsson F., Radic V., Sigurðsson O. and Thorsteinsson Th. 2006. The impact of climate change on glaciers and glacial runoff in the Nordic countries. Proc. The European Conference of Impacts of Climate Change on Renewable Energy Sources, Reykjavík, Iceland, June 5–6. Jóhannesson, T., Aðalgeirsdóttir G., Björnsson H., Crochette P., Elíasson E. B., Guðmundsson S., Jónsdóttir J. F., Ólafsson H /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 29. esa_flyer_new

  EA Analyse A/S and Optensys Energianalys will forecast energy system variables, while SINTEF Energy Research will make assumptions for the energy system in different cases, include new inputs in the EMPS model and carry out simulations. Cl i ma t e Sc e nar i os G ro u p R i s ø St o c h as t i c v a r i a b l e s Clima t e s c e n a r i o NV E S M H I FE I N o r w a y S w e d e n F inla n /media/ces/esa_flyer_new.pdf

• 30. 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