32 results were found for WA 0821 7001 0763 (FORTRESS) Pintu Baja Mother And Son Alor Selatan Alor.

Results:

21. VI_2021_008

/media/vedurstofan-utgafa-2021/VI_2021_008.pdf
22. Hare-2011-ParticipatoryModelling

ea th , th e m et ho d u se d at th is st ag e fo r th es e st ak eh o ld er typ es is sp ec ied .Sh oul d ther e be tw o o r mor e model sbein g develope d in th e process ,the n th e typ e o fmode lt o whic h th e metho d wa s applie d is show n in parentheses .O T re fe rs to th e co m po si tio n o ft he o rg an iz in g te am . Fo r o rg an iz in g te am in vo lve m en t in di ffe re n t pa rt /media/loftslag/Hare-2011-ParticipatoryModelling.pdf
23. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

the different realizations of climate change are not independent. The first four rows of Figs. 3.4 and 3.5 show the diagnosed geographical distributions of a, b, and 0 for temperature and precipitation change in the four three month-seasons (DJF = December-January-February, MAM = March-April-May, JJA = June-July-August, SON = September-October-November) and for the annual mean /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf
24. VI_2022_006_extreme

months are abbreviated to first letters. RCP 2.6 Percentage change (%) 2040 - 2060 2080 – 2100 10th 50th 90th 10th 50th 90th DJF -12 1 17 -14 2 20 MAM -12 4 23 -13 3 22 JJA -12 3 21 -13 4 24 SON -9 4 21 -9 5 21 Annual -11.3 3 20.5 -12.3 3.5 21.8 RCP 8.5 Percentage change (%) 2040 - 2060 2080 – 2100 10th 50th 90th 10th 50th 90th DJF -11 2 21 -15 3 27 MAM -13 3 21 -15 5 23 JJA -11 3 /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf
25. VI_2020_004

/media/vedurstofan-utgafa-2020/VI_2020_004.pdf
26. VI_arsskyrsla2020

Monitoring and risk assessments were revolutionized in 1997 in the wake of avalanches that claimed lives in Súðavík and Flateyri in 1995. In 2004, a Centre for ava- lanche monitoring, risk assessments and research was established in Ísaörður and continues to prove the value of its existence. Harpa Grímsdóttir snjóflóðasérfræðingur og Oddur Péturs- son snjóeftirlitsmaður við opnun snjóflóðaseturs á /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf
27. GA_2009_91A_4_Andreassen

and manyof the individual snow falls in late summer (Fig. 4).However, much of the variability in the winter sea- son was not reproduced by the model, but thesealbedo fluctuations have little impact on the net bal- ance as the energy available for melt is seldom pos-itive in the winter months. Ice albedo was assumedto be constant, a value of 0.30 was chosen. Meas-urements from the AWS as well as the point /media/ces/GA_2009_91A_4_Andreassen.pdf
28. Water_resources_man_Veijalainen_etal

in Lake Pielinen and Lake Saimaa (Table 2), but the seasonal changes were significant (Fig. 4). The water levels increased during winter and decreased during summer months. Student t-tests for the average seasonal (winter [DJF], spring [MAM], summer [JJA], autumn [SON]) water levels showed that in 2040–2069 and 2070–2099 the changes in water levels from the reference period were on average /media/ces/Water_resources_man_Veijalainen_etal.pdf
29. Eriksson_Garvill_Nordlund_2006

¨lle (2003) demonstrate a relation between perceived freedom and perceived fair- ness; the larger the infringement on freedom the less fair road pricing is perceived to be. Expected own reduction in car use, as a consequence of the TDM measure, is another belief reflecting effects on the individual car user. Jakobs- son et al. (2000) found own reduction to be directly related to perceived fairness /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf
30. VI_Arsskyrsla_2018_vef

ný viðfangsefni sam- einaðrar stofnunar. Til þessa verks voru fengnir þrír sérfræðingar, Einar Sveinbjörns- son veðurfræðingur, Hákon Aðalsteinsson vatnalíffræðingur og Sveinbjörn Björnsson eðlisfræðingur og leiddi hann hópinn. Sér- fræði hópurinn skilaði ítarlegri álitsgerð um starfsemi stofnan anna og kosti sameiningar. Í framhaldi af framangreindri greiningar vinnu skipaði umhverfisráðherra /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf