80 results were found for WA 0821 7001 0763 (MEVVAH) model marmer dinding P. Haruku Kabupaten Maluku Tengah Maluku.

Results:

• 41. Seismic signal associated with the Askja rockslide

  is characteristic for a surface wave. As no body waves are seen prior to the low frequency onset, this event clearly differs from a normal tectonic earthquake which usually starts with clear onsets of P- and S-waves prior to the surface waves. Figure 2 Interpretation The preliminary interpretation of this signal is that the low frequency waves in the beginning reflect a slow rupture process /earthquakes-and-volcanism/articles/nr/2921

• 42. 2010_003rs

  plate spreading motion, according to the NUVEL-1A plate motion model (DeMets et al., 1990, 1994). Using a simple screw dislocation model to interpret GPS campaign measurements on the RP from 1993 and 1998, Hreinsdóttir et al. (2001) suggested that rifting on the peninsula occurred in pulses, since their research indicated present accumulation of left-lateral shear strain parallel to the peninsula /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 43. The magma path revealed

  seismicity near to the eruption site in the morning of the 21st. On the vertical section viewed from the south two velocity models are shown, the SIL-model (black lines) used for the automatic and daily manual location processes, and the improved South-Iceland model (P23, green lines) used in the relocation process. Thin lines show S-wave velocity and thick lines show P-wave velocity. Eruption site /about-imo/news/nr/1859

• 44. norsem_korja

  fault zone in the Kuusamo area, the gradient seems to be associated with a zone of increased seismicity. In these areas, the crustal thickness gradients are optimally oriented for reactivation. Because the spatial distribution of the registered earthquakes exhibits little to no correlation with the an existing ellipsoidal rebound model or Glacial Isostatic Adjustment (GIA /media/norsem/norsem_korja.pdf

• 45. Kurpniece_Liga_CES_2010

  From 1925 to 1938, Aiviekste HPP was the largest in Latvia. Daugava and Aiviekste Basins Study area After Plavinas HPP was constructed in 1967, territories near Plavinas city and above river to Jekabpils city almost every spring are endangered by floods caused mostly by ice jams. Hydrological model • since year 1994, HBV model is used at LVGMC • HBV 96 model (version 4.5) was used to simulate /media/ces/Kurpniece_Liga_CES_2010.pdf

• 46. GA_2009_91A_4_Andreassen

  ). This impliesthat a 1°C warming must be compensated by a30% increase in precipitation to avoid mass defi- cit. The sensitivity to a 1°C decrease in tempera-ture was +0.47 m w.e., thus the climate sensitivity of ±1°C is 0.55 m w.e. A decrease in precipitation of 10% reduced the bn by 0.21 m w.e, the resultingclimate sensitivity to ±10% P is 0.20 m w.e. Model results revealed that the day of maximum bw /media/ces/GA_2009_91A_4_Andreassen.pdf

• 47. Dataseries and components

  ), quantity (mm), pH Heavy metals in aerosol: Pb, Cd, Cu, Zn, Cr, Ni, Fe, Mn, V, As, Al (ng/m3) Cl, NO3-N, SO4-S (µg/m3) Hg (pg/m3) Persistent organic pollutants (POPs), same for precipitation (ng/l) and air (pg/m3): alfa-HCH, beta-HCH, gamma-HCH p,p'-DDE p,p'-DDD o,p'-DDT p,p'-DDT dieldrin HCB cis-chlordan, trans-chlordan, trans-nonachlor, PCB-28, -31, -52, -101, -105, -118, -138, -153, -156 /pollution-and-radiation/pollution/components/

• 48. Risk Assessments

  (2009) Test and evaluation of climate risk/opportunity assessment approach. Case study: biomass fired CHP plant, Jämtkraft, Sweden. IVL, Swedish Environmental Research Institute. February-March 2009. 14 p. James-Smith, Edward (2009) Risk analysis for transmission and distribution of power in changing climatic conditions. EaEA. Ea Energy Analyse. 11 p. Keränen, Jaana (2009) Vesivoimalaitosten /ces/publications/nr/1941

• 49. VI_2020_005

  sinking. This was estimated from an assumed absolute sea level rise along with relative sea level trends. However, an underestimation of land uplift is probable in these assessments (Madsen, 2009). A land uplift model for Denmark produced by DTU Space with GNSS data from Geodatastyrelsen, precision levelling and the Danish Meteorological Institute’s water level data, shows land uplift of just under /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 50. VI2010-006_web

  /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf