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mass (see Fig. 1). To evaluate the accuracy of control runs, model
results are compared with mean monthly fields on 1 1-degree grids obtained from the ERA-40
reanalysis project (Uppala et al., 2005). To that end, the 20th Century GCM runs are restricted to
the 1958–98 control period, that is covered by all models, as well as the ERA-40 reanalyses.
To decrease the uncertainty of future climate
/media/ces/2010_005_.pdf
10. Rake distribution for mapped faults/clusters in box J, Hella. ........................ 97
Figure B.11. Rake distribution for mapped faults/clusters in box K, Hraungerði. ............. 97
Figure B.12. Rake distribution for mapped faults/clusters in box L, Skeið. ........................ 98
Figure B.13. Rake distribution for mapped faults/clusters in box M, Land. ....................... 98/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
236
1992 09 167 124 167 98
1995 07 1994 1759 599 368
1995 10 96 62 73 37
1997 07 921 728 330 184
2000 08 1240 1083 365 221
2002 09 689 582 267 160
2003 11 241 207 139 98
2006 04 1370 1340 300 270
2008 10 1350 1290 300 265
The origin of the 1957, 1960, 1964 and 1966 jökulhlaups is not certain but is most likely the eastern cauldron. The discharge
and volume for the 1995 jökulhlaup are a sum from
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
1
PhD Workshop preceding Adaptation Research Conference – 27 & 28 August, Helsinki
Climate change adaptation - Analysis, Planning and Implementation
Programme
Venue: Rantapuisto, Ramsinniementie 14, FIN-00980 HELSINKI
directions for travel can be found at the conference web site
http://www.nordicadaptation2012.net/
Informal start at 26 August
On Sunday evening 8pm an informal get
/media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
–3736.
Jenkinson, A.F. (1955). The frequency distribution of the annual maximum (or minimum) of
meteorological elements. Quart. J. R. Met. Soc. 81, 158–171.
Jingyi, Z. & Hall, M.J. (2004). Regional flood frequency analysis for Gan-Ming river basin in
China. J. Hydrol., 296, 98–117.
Kjeldsen, T.R. & Jones, D. (2007). Estimation of an index flood using data transfer in the UK.
Hydrol. Sci. J., 52(1
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf
aversion should influence the first mover’s decision. The
98 Public Choice (2012) 151:91–119
Fi
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1
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Public Choice (2012) 151:91–119 99
Table 1 The predicted effect of
intrinsic preferences on first and
second movers’ contributions
1st mover 2nd mover
Disadvantageous Negative None
inequity aversion
Advantageous None Positive
inequity
/media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf
were more opposed to this TDM measure compared to the increase
with two SEK/liter (F ð1; 902Þ ¼ 4:98, po0:05, partial Z2 ¼ 0:005).
Significant differences were found between all the examined
evaluations of the three TDM measures. Increased tax on
fuel was expected to infringe on freedom to choose travel
mode to a larger extent compared to the information
campaign. Improved public transport
/media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf