89 results were found for 【K528.COM】X账号购买平台 kx9qd.

Results:

• 51. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  296 Public Choice (2010) 143: 293–301 2 The commons The literature on the commons, or what is more technically defined as common-pool re- sources (CPRs), should be viewed initially from its place in the larger literature on dilem- mas of collective action. Since the foundational work of H. Scott Gordon (1954) on the com- mons, and Mancur Olson (1965) on collective action more broadly, the behavioral /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 52. VI_2019_009

  with the following equation, h = c t 2 where c is the speed of light (c = 2.99 x 108 m/s). In principle, CL51 is able to detect three cloud layers simultaneously, but if the cloud base is obscured due to precipitation or ground-based fog, vertical visibility is reported. Information about fog and precipitation can also be derived from the return signal as they attenuate the return signal from a cloud. In its /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 53. 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

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

  + x−k) (1) Public Choice (2012) 151:91–119 95 with k = 1,2, and −k = 1 if k = 2, −k = 2 if k = 1. The variables xik and x−k are the contributions to the public good of subject i as mover k and mover −k, respectively. The contribution of the first mover is an integer x1 ∈ [0,10] and that of the second mover takes one of the two values x2 ∈ {0, x1}. 2.2 Theoretical predictions As noted /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.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

• 56. CES_D2.4_task1

  distribution of anthropogenic climate changes, largely following Räisänen and Ruokolainen (2008a,b). The main features of this procedure are as follows: x Model simulations of 20th and 21st century climate change are used to develop linear regression equations that relate the local temperature or precipitation climate to a smoothed (11-year running mean) evolution of the global mean /media/ces/CES_D2.4_task1.pdf

• 57. VI_2017_009

  we take the corresponding data from the CMIP5 project. Table 1. All GCMs and RCMs used in this study. If a model is available for any of the domains Arctic-44, EURO-44, or EURO-11, it is marked with a v, but with an x if it is unavailable. Model name Type EURO-11 EURO-44 Arctic-44 CCCma-CanESM2 GCM x v v COSMO-CLM4-8-17 RCM v v x CNRM-CERFACS-CNRM-CM5 GCM v v x IHCEC-EC-Earth GCM v v v /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 58. 2005EO260001

  level in Skeidará waned. The last sign of a crater explosion was seen at GRF early on 6 November, leaving only a weak tremor signal from the remnants of the jökulhlaup. The jökulhlaup fi nally ended in early December, after ~0.8 km3 of water had drained from the Grímsvötn lake (J. Hardardóttir, personal com- munication, 2005). Location and Volume Constraints Earthquake locations at Grímsvötn /media/jar/myndsafn/2005EO260001.pdf

• 59. Paper-Olafur-Rognvaldsson_92

  a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 60. vonKorff_etal-2010

  finished, and possibly tested before implementation starts (Bots 2007). Following Bots (2007), we note that the word “design” can denote an activity as well as a product. In this article, design as a product is synonymous with the participation plan (point y). This plan is based on design as an activity, represented here by the space between points x and y. What needs to happen in this phase (x /media/loftslag/vonKorff_etal-2010.pdf