Warning
There are indication that magma has started moving underneath Svartasengi and an eruption is likely to occur within an hour or so.

72 results were found for 菲律宾圣安娜假盘菲律宾圣安娜假线【191-1999-2299】圣noiw安Fc2kG.

Results:

61. Refsgaard_etal-2007-Uncertainty-EMS

and possibly the stake- holders at different phases of the modelling project. Many QA guidelines exist such as Middlemis (2000) and Van Waveren et al. (1999). The HarmoniQuA project (Schol- ten et al., 2007; Refsgaard et al., 2005a) has developed a com- prehensive set of QA guidelines for multiple modelling domains combined with a supporting software tool, MoST (downloadable via http /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
62. VI2010-006_web

fyrir snjóflóðahættumat undir lágum bökkum eins og Akureyrarbrekkum (Tómas Jóhannesson, 2009). Í þessum viðmiðunarreglum eru áhættureikningar fyrir hefðbundna snjóflóðafarvegi, sem eru nokkur hundruð metra háir eða hærri (Kristján Jónasson o.fl., 1999), aðlagaðir að lægri hraða sem vænta má að snjóflóð nái þar sem fallhæð er einungis nokkrir tugir metra. Hættumatið fyrir Akureyri byggist þrátt /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf
63. 2011_005

a continuous GPS network (ISGPS) in 1999 for monitoring and research of crustal deformation as a primary purpose. Since then the institute has been leading in operating continuous GPS stations in Iceland. A total number of 64 continuous GPS stations were in operation in Iceland at the beginning of 2010, of those the Icelandic Meteorological Office was responsible for operating 58 /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf
64. 2010_016

temperature, precipitation and discharge variation to the 1981–2000 means was used to confirm the selection. For Sandá í Þistilfirði the years 1962, 1989, and 2001 were selected and for Austari-Jökulsá 1975, 1977, and 1999 were selected. Median, max and min changes of temperature and precipitation predicted by the thirteen different climate scenarios for each of the meteorological station used /media/ces/2010_016.pdf
65. VI_2014_001

flood method for deriving flood quantiles at gauged sites with limited data availability (see for in- stance Blazkova and Beven, 1997; Cameron et al., 1999; Fiorentino et al., 2007; and a review by Boughton and Droop, 2003). A distributed hydrological model calibrated on a gauged catch- ment can be used to continuously simulate discharge series at different sites on that catchment and flood /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf
66. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
67. VI_2015_005

(2012) based on an EOF analysis of ERA-40 data, for the winters (DJF) during the 1958 – 1999 period. The northeast- to-southwest anomaly gradient across the northern North Atlantic accompanies a strong polar vortex, with weak meridional but strong westerly flow at mid- and upper-levels across the ocean and into Western Europe. The no-cyclone mode is similar to the negative North Atlantic Oscilla /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
68. VI_2009_002rs

/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_002rs.pdf
69. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
70. VI_2013_008

(Radinovic´, 1975; Kruizinga & Murphy, 1983; Van den Dool, 1989; Fraedrich et al., 2003) and climate downscaling (Zorita & Von Storch, 1999; Wetterhall et al., 2005) to extract local weather information which can not be simulated by coarse-resolution meteorological or climate models with sufficient accuracy. In that context, these methods often make use of synoptic predictors describing /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf