47 results were found for Investire senza paura di truffa con JZMOR: la guida definitiva.

Results:

• 1. IPPC-2007-ar4_syr

  or as a result of human activity. This usage differs from that in the United Nations Framework Con- vention on Climate Change (UNFCCC), where climate change refers to a change of climate that is attributed directly or indi- rectly to human activity that alters the composition of the global atmosphere and that is in addition to natural climate variability observed over comparable time periods. Warming /media/loftslag/IPPC-2007-ar4_syr.pdf

• 2. IMO_AnnualReport2014

  probably a few meters. An interactive 3D model of the earthquakes during the magma intrusion. The di?rent colours represent the activity in time from 16 August to 12 September. During the magma intrusion, intense earthquake activity related to subsidence of the Bárðarbunga caldera was located at the caldera rim. Over 70 earthquakes above magnitude 5 occurred in the first four months after the onset /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 3. Hare-2011-ParticipatoryModelling

  is ar tic le X X X X X X X Identif ygenera lform so f pa rt ici pa to ry m o de llin g Tabl e1 . Co m pa ris o n o ff ra m ew o rk s fo r ca te go riz in g pa rt ic ip at o ry m o de llin g pr o ce ss es . Th is ta bl e co m pa re s di ffe re n tf ra m ew o rk s (bo ld , fir st co lu m n )a cc o rdin gt o th e categorica lcriteri a the yemplo y(column si n italics )an d thei rpurpos e (bold ,fina /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 4. Refsgaard_etal-2007-Uncertainty-EMS

  specified in the model study plan. Con- sideration must be given to the spatial and temporal detail required of a model, to the system dynamics, to the bound- ary conditions and to how the model parameters can be de- termined from available data. The need to model certain processes in alternative ways or to differing levels of detail in order to enable assessments of model structure uncer- tainty should /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 5. Adalgeirsdottir-etal-tc-5-961-2011

  expeditions to this area were con- ducted in 1936–1938, when a group of Swedish and Ice- landic glaciologists measured ice flow, surface mass balance and surface topography. They also carried out a detailed analysis to understand the relative roles of accumulation and melting in the total mass balance of the glacier and to estab- lish a relationship between the climate and the advance and retreat /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

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

  to meet the challenge of navi- gating nature’s dynamics’’ and conclude that ‘‘learning how to sustain social-ecological systems in a world of continuous change needs an institutional and social con- text within which to develop and act’’. Knowledge and the ability to act upon new insights are continuously enacted in social processes. The social network of stakeholders is an invaluable asset /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 7. VI_2016_006_rs

  in a collaboration between the Austrian engineering company Ingenieurbüro Illmer Daniel e.U. (DI), Efla consulting engineers and the Icelandic Meteorological Office (IMO). Daniel Illmer carried out the analysis of landslide protection measures, Jón Kristinn Helgason, Tómas Jóhannesson and Eiríkur Gíslason wrote sections about the geographical setting, the land- slide history and the assessment /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 8. 2013_001_Nawri_et_al

  in a vertical plane, this is the component of the three-dimensional flow relevant for wind energy assessments. 13 The simulated data provide a good overview for the whole island. However, with a grid-point spacing of 3 km, the WRF model results are too coarse for a precise assessment of the wind con- ditions within a limited region, such as an individual valley or ridge, that may be appropriate /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 9. GA_2009_91A_4_Andreassen

  whenmonthly lapse rates are applied instead of a con-stant lapse (Fig. 3b). Note that although the r values are similar, the annual lapse rate produces far toohigh temperatures in summer. Furthermore, tem-peratures at Fokstugu are sometimes significantly lower in winter compared to the AWS, probablydue to less mixing of the air at Fokstugu than on theglacier.We also calculated mean summer /media/ces/GA_2009_91A_4_Andreassen.pdf

• 10. Lorenzoni_Pidgeon_2006

  of geographical and cultural elements on perceptions of climate change and how, although individuals expressed concern about future undesirable consequences of climate change impinging on the national good, this did not exclude them from con- sidering the potential personal benefits deriving from future changes in the climate (Palutikof et al., 2004, in the UK, Galeotti et al., 2004, in Italy /media/loftslag/Lorenzoni_Pidgeon_2006.pdf