87 results were found for 【K06.CC】推特老号购买,x号购买 sdent.

Results:

• 41. Kok_1-scenarios-lecture-1

  .. But with caution Spatial scale Modifiable Areal Unit Problem (MAUP) Ecological fallacy: The mistake of assuming that where relationships are found among aggregate data, these relationships will also be found among individuals or households, or vice versa. Key concepts (from ecology) Forest cover Population density y = -20.1Ln(x) + 60 R2 = 0.84 0 20 40 60 80 100 0 5 10 15 Population density F o re /media/loftslag/Kok_1-scenarios-lecture-1.pdf

• 42. raisanen_ruosteenoja_CES_D2.2

  as the forecast period. On the other hand, the probability distributions derived using the resampling ensemble method are in most cases wider than those produced with the normal distribution method, particularly so for precipitation change. This difference stems from the different treatment of natural variability: x In the normal distribution method, all simulations available for the same emission /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 43. Alam_Ashraful_CES_2010

  (ECT) Working paths and machinery transportation + C Rotation period Plant production and transportation Site preparation a r b o n Planting E n e r d i o Thinnings/ harvesting operations h di g y i x i d e Emission parametersEcosystem model S ort stance transportation Long distance n p u t E m i s Emission calculation tool transportation Chipping s i o n CO2 balance 14 Energy wood /media/ces/Alam_Ashraful_CES_2010.pdf

• 44. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  et al .( 200 4) 21 .Explici tconsideratio n o funcertaint y (relate dt o CC impacts ) Uncertaintie s ar e no t glosse d ove r bu tcommunicate d (in fina lreports ,orally ) Diet z et al .( 200 3), Brugnac h et al .( 200 8) Researcher s ar e willin g to tal k wit h stakeholder s abou tuncertaintie s Diet z et al .( 200 3), Brugnac h et al .( 200 8) 22 .Broa d communicatio n (on CC impacts /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 45. Gradual fading of seismic activity at Bárðarbunga and the dyke intrusion

  with the general observation of a slowly fading activity in almost all other data sets. Inter-event waiting time For the Bárðarbunga caldera, inter-event waiting time for earthquakes equal to or larger than M5 has been plotted* during the four months period from the onset of events until 15 Dec 2014. On the y-axis, waiting time is given in hours. The x-axis shows the relevant earthquakes /earthquakes-and-volcanism/articles/nr/3039

• 46. 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

• 47. 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

• 48. 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

• 49. 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

• 50. Perrels-CBA

  enhanced weather effects on road infrastructure • traffic safety • road maintenance • traffic capacity • Assessing flood risks in cities • TOLERATE: From climate modeling to appraisal of counter measures • IRTORISKI: Extended event-tree analysis Next pages (EWENT) 26.8.2011Adriaan Perrels/IL 26 Road capacity effects of weather & CC Changes in the supply curve caused by extreme weather conditions /media/loftslag/Perrels-CBA.pdf