65 results were found for การจัดอันดับ Google Output(TG:e10838).zsu.

Results:

• 51. Reykholt-abstracts

  /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 52. 2011_005

  different data types and where they are stored. Table 14. Different types of data and storage locations. Data type Location Receiver files dump*, eldvarp, jar, rek, rek2, and several SIL stations RINEX and qc data dump Receiver voltages and temperature dump Time-series data lapis Processing logs lapis Graphical output hraun (via ris.vedur.is) *Incomplete record: data from 2010 /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf

• 53. Update on activity in Eyjafjallajökull 2010

  at Þorvaldseyri, just south of the eruption site. Noise was reported from Vestmannaeyjar-islands (35-40 km southwest of erutpion), Vatnsdalur (190-200 km to the north), and Borgarfjörður (~150 km to the northwest). Deflation of the Eyjafjallajökull volcano contiues. Compared to last seven days, the output from the volcano has been slowly decreasing but the activity has been pulsating and further changes /earthquakes-and-volcanism/articles/nr/1884

• 54. 2010_016

  in the derivation of scenarios for short term climate change impact assessments. The most important are: Type of scenario. Typical δ-change scenarios have various flaws. For example they do not preserve the variability from regional climate models, but only resample the internal variability of former climate used as base. Direct model output is, however, often difficult to use because of biases that make /media/ces/2010_016.pdf

• 55. VI_2014_005

  such that initial and boundary conditions, for each forecast run, are combined with the last output from the previous run (ANAATMO=blending). Gridded surface analyses for 2-m air temperature and relative humidity, sea surface temperature, and snow water equivalent are prepared by the spatial interpolation tool CANARI (ANASURF=CANARI_OI_MAIN). The model is run uninterrupted for an entire hydrological year /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 56. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  that were available in the ENSEMBLES Research Theme 3 data base 6 in mid-June 2009 and (i) had been run at 25 km resolution for the A1B scenario (ii) in a domain considered sufficiently large for our analysis, and (iii) for which no technical problems were detected in an initial inspection of the model output. The data for most of the RCMs were available as interpolated to a regular 0.25° × 0.25 /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 57. raisanen_ruosteenoja_CES_D2.2

  associated with such a local analysis, it should be stressed that these results are based on output from relatively coarse-resolution global climate models. These models are not skilful in simulating such small-scale features in climate change that might be associated with the details of the regional land-sea distribution and orography (the effects of which are expected to be captured better by regional /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 58. VI_2022_006_extreme

  Intercomparison Project (CMIP) is a large framework that collects the output from global coupled ocean-atmosphere general circulation models (GCMs) to project future climatic changes due to anthropogenic activity. For this project, results from the fifth 10 phase of the project (referred to as CMIP5; for details, see Taylor et al., 2012) are used based on two different greenhouse gas /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

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

  characterized by two dif- ferent management paradigms—management as control versus management as learning—are contrasted as the extreme, opposing ends of six axes. Interdependence of the regime characteristics and responsiveness to floods and droughts The key objective of our research is to see whether there is a link between regime characteristics and responsiveness to floods and droughts (as an output /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 60. Hare-2011-ParticipatoryModelling

  mapping was used to elicit individual stakeholder perspectives regarding the existing management system. If one considers the model output of Hase II to have been the integrated conceptual model, then, in contradiction of Bots and van Daalen (2008), the model construction stage was not carried out using cognitive mapping, but involved the stakeholders doing group model building, using the cognitive maps /media/loftslag/Hare-2011-ParticipatoryModelling.pdf