31 results were found for WA 0821 7001 0763 (FORTRESS) Pintu Baja Fortress Mom And Son Muncang Lebak.

Results:

21. 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
22. 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
23. 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
24. VI_2020_004

/media/vedurstofan-utgafa-2020/VI_2020_004.pdf
25. 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
26. 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
27. 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
28. 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
29. 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
30. VI_2013_008

In Iceland, floods are primarily of three different origins (Snorra- son et al., 2012): (i) meteorological floods induced by rain and which are often combined with melting of snow and ice, (ii) floods due to ice formation and release within river channels, and (iii) glacier outburst floods which originate in marginal lakes, formed in glacier dammed side valleys, or subglacial lakes, formed as a result /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf