Note
Earthquake swarm occurring east of Grímsey, biggest earthquake of M5.0.

48 results were found for 日本の検索エンジン 🔍 www.81.biz.

Results:

31. 2010_017

) [hours] kD (from hydro- graph) [hours] kI (opti- mized) [hours] kI (from hydro- graph) [hours] R2 R2log MPE annual [%] RMSE annual [m3/s] MPE daily [%] RMSE daily [m3/s] Austari- Jökulsá, vhm 144 Without g.w. module 81 20–50 5000 120–240 0.65 0.66 2.3 4.0 7.9 14.1 With g.w. module 50 20–50 150 120–240 0.68 0.75 5.5 3.7 9.1 13.6 Sandá í Þistilfirði /media/ces/2010_017.pdf
32. VI_2020_004

-based maps ............................................................................ 81 5.4.5 Probability of exceedance and accumulation rate ............................................ 87 5.5 Towards an integration of the three explosive eruptive scenarios ............................. 93 6 Main conclusions and next steps /media/vedurstofan-utgafa-2020/VI_2020_004.pdf
33. 2010_003rs

on the Reykjanes Peninsula (boxes B-F). .................................................................... 81 Table A.3. Fault parameters for mapped fault segments and clusters in the Hengill area and the South Iceland seismic zone (boxes G-I). ..................................... 82 Table A.4. Fault parameters for mapped fault segments on the Hestvatn fault (J-21) (box N /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
34. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

/media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf
35. Gudmundsson-etal-2011-PR-7282-26519-1-PB

). The ice caps are Eyjafjallajo¨kull (ca. 81 km2), Tindfjallajo¨kull (ca. 15 km2) and Torfajo¨kull (ca. 14 km2). The DEMs were compiled using aerial photographs from 1979 to 1984, airborne Synthetic Aperture Radar (SAR) images obtained in 1998 and two image pairs from the SPOT 5 satellite’s high-resolution stereoscopic (HRS) instrument acquired in 2004. The ice-free part of the accurate DEM from 1998 /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
36. VI_2015_009

J.R.M., Wallis, J.R. & Wood, E.F. (1985b). Estimation of the generalized extreme- value distribution by the method of the probability-weighted moments. Technometrics, 27(3), 251–261. Jenkinson, A.F. (1955). The frequency distribution of the annual maximum (or minimum) of meteorological elements. Quart. J. R. Met. Soc. 81, 158–171. 24 Malekinezhad, H., Nachtnebel, H.P. & Klik, A. (2011a). Comparing /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
37. Eriksson_Garvill_Nordlund_2006

/media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf
38. Kok_et_al._TFSC_published_2011

/media/loftslag/Kok_et_al._TFSC_published_2011.pdf
39. Lorenzoni_Pidgeon_2006

or no effect on them (Kirby, 2004). Among some Germans interviewees, climate change also had “a lower cognitive presence”, being overshadowed by other events which are more directly experienced and important to everyday life (Ho¨hle, 2002, p. 117). PUBLIC VIEWS ON CLIMATE CHANGE: EUROPEAN AND USA PERSPECTIVES 81 Elicitations of views on climate change relying on past events as analogues for future /media/loftslag/Lorenzoni_Pidgeon_2006.pdf
40. Refsgaard_etal-2007-Uncertainty-EMS

/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf