35 results were found for 화전역건전마사지♤텔레 GTTG5♤繯화전역남성전용鹊화전역딥티슈ן화전역딥티슈출장鄹화전역로미로미🚇correlation/.

Results:

• 11. ces_SA_group_flyer_new

  analysis of variability and uncertainty in extreme events, statistical methods for dam safety, long-term patterns of precipitation extremes, seasonal and inter- annual variations in wind and streamflow and their dependence on large-scale circulations patterns. Correlation coefficients for annual wind speed /streamflow with the NAO /media/ces/ces_SA_group_flyer_new.pdf

• 12. Karlsdottir-Risk_analysis_IMO_SK

  of the flood  how fast does floods reach inhabited areas Probabilities of volcanic eruptions in the area return period is there a correlation between the strength of the eruption and return period Information on preperdness issued to residents in the area Information to tourists in different languages Information posters at touristic sites Hekla ... Exercises held 2006 a two day exercise in the area /media/loftslag/Karlsdottir-Risk_analysis_IMO_SK.pdf

• 13. VI_2015_005

  pressure, in a diverse geographical setting, is related to local temporal fluctuations of precipitation, and to 11 Figure 4. Coefficient of determination, with the sign of correlation, between mean sea level pressure and total daily precipitation in winter and summer, for grid-point time-series of daily averages (top row), and for 5-day running means of daily time-series (bottom row). the zonal component /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

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

  as a ref- erence map for co-registering the SPOT5 HRS-DEM (pixel resolution of 40× 40 m), using the ice free areas surround- ing Hoffellsjökull and the correlation method described by Guðmundsson et al. (2011). This comparison revealed a hor- izontal shift of the HRS-DEM by 15 m and 5 m towards east and north, respectively, and a vertical offset of 2.3 m. Gaps in the HRS DEM, due to low contrast /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 15. Journal_of_Hydrology_Veijalainen_etal

  from 1971 to 2000 as input. The simulated floods in 2010–2039 and 2070–2099 will be compared to these simulated floods of the reference period. The fit of the Gumbel distribution to observed annual maximum discharges of 1971–2000 was estimated with two goodness of fit tests; the chi-square test (e.g. Kite, 1977) and the probability plot correlation coefficient test statistic (Heo et al., 2008 /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 16. VI_2009_012

  correlation between log distance and magnitude can result in large errors in the fitted parameters a and b. In their paper, Fukushima and Tanaka (1990) argue that a high correlation between log distance and magnitudes are responsible for consistently low distance parameters in older Japanese attenuation studies. Using a one step regression model, their distance parameter, a, was estimated as 1.19 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 17. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

  are heterogeneous in their degrees of inequity aversion: 17.8% of the 118 subjects are purely selfish (α = β = 0) and 39.8% are averse to both advantageous and disadvanta- geous inequity (β > 0 and α > 0). Advantageous and disadvantageous inequity aversion are not correlated (Spearman correlation test: z = 0.0265, p = 0.7758).20 Figure 2 depicts the distribution of advantageous and disadvantageous inequity /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 18. Eriksson_Garvill_Nordlund_2006

  orientation is positively related to problem awareness and personal norm, furthermore problem awareness has a positive association with personal norm and willingness to reduce car use. In turn, a positive correlation between personal norm and willingness to reduce car use for environmental reasons is expected. In the second part of the model, willingness to reduce car use is expected to be related /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf

• 19. VI_2021_008

  request. In addition to this new and improved web-based plotting program, there is a new web portal accessible to all research staff at the IMO to request and download csv RSAM data (see Figure 16). Currently, the web page can provide RSAM data from 1996 to the present day. This tremor data can be easily plotted with other volcano monitoring and meteorological data to observe the correlation /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 20. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  in position and a vertical accuracy better than 5 m in ice-free gentle relief areas and 10 m at higher relief areas with slopes less than 20% (Bouillon et al. 2006; Berthier & Toutin 2008). A mask including stereo image correlation scores was delivered as a SPIRIT bi- product and used in this study to exclude uncorrelated pixels from the DEM. We constructed the 2004 October 5 SPOT 5 HRS DEM using /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf