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

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• 11. Eyjafjallajokull_status_2010-05-09_IES_IMO

  to yesterday. Seismic tremor: Has been similar for the past 3 days, and similar amplitude on all frequency bands. Earthquakes: Seven earthquakes of magnitude 1.5-2 have been located for the last 24hrs. GPS deformation: Horizontal displacement towards the center of Eyjafjallajökull volcano and subsidence. Overall assessment: Compared to last seven days, the output from the volcano has /media/jar/Eyjafjallajokull_status_2010-05-09_IES_IMO.pdf

• 12. IMO and The Icelandic Civile Protection Agency reassess the status for

  stable values. Measurements in late March indicate that the geothermal heat output beneath the cauldron has diminished significantly from what is was when the cauldron formed. There is a possible small, ongoing inflation signal in Öræfajökull, however there are no signs of an imminent eruption.The uncertainty phase declared by the Icelandic Civil Protection and Emergency Management remains /about-imo/news/the-imo-and-the-icelandic-civile-protection-agency-reassess-the-status-for-oraefajokull

• 13. Paper-Olafur-Rognvaldsson_92

  model output is used as input to the WaSiM hydrological model to calculate and compare the runoff with observed runoff from six watersheds in Iceland. It is found that model results compare favourably with observations. INTRODUCTION The 6–hourly ERA40 re-analysis of the ECMWF have been dynamically downscaled for the period 1961–2006 using the numerical model MM5 (Grell et al., 1995). The modelling /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 14. PhD Workshop 2012

  or 3 lectures of 45 minutes from international specialists on climate change adaptation. As a concrete output of the group work, a selection of PhD students will be offered the opportunity to make a short plenary presentation during the conference. citation from conference website /nonam/adaption/phd-workshop-2012/

• 15. Machguth_Horst_CES_2010

  balance scenarios: • correct several parameters in several dimensions • large amount of data needed • more simple methods? • e.g. general trends from climate-model ensembles superimposed to measurements Thank You We greatly acknowledge the Rossby Center and Ralf Döscher for providing us with the RCAO output and DMI for the HIRHAM4 data Thomsen and Reeh (1986) /media/ces/Machguth_Horst_CES_2010.pdf

• 16. CES_D2.4_solar_CMIP3

  global radiation), i.e., the sum of the direct and diffuse solar radiation. The quantity can be expressed in W/m2 or MJ/m2 per time unit. In this account, changes in incident radiation are viewed both in absolute1 and percentage terms. Model output data were downloaded from the CMIP3 data archive. There were a few models for which the simulation for one of the three scenarios was missing; in those /media/ces/CES_D2.4_solar_CMIP3.pdf

• 17. Lettenmaier_Dennis_CES_2010pdf

  interpolated to VIC scale Regional Bias: spatial example GSM: NCEP Global Spectral Model obs prcp GSM prcp obs temp GSM temp JULY Verification using NCEP Global Spectral Model (GSM) output Process into the daily VIC-scale input time series Force hydrology model to produce streamflow Ohio R. flow @ Metropolis, IL Start with GSM-scale monthly observed T & P (“unbiased”) time series /media/ces/Lettenmaier_Dennis_CES_2010pdf.pdf

• 18. The second CES Workshop, held at SMHI in Norrköping, Sweden, May 2008

  precipitation and runoff to 2050. New time series for the Baltic countries will be developed within CES project. Statistical downscaling and adjustment of RCM-output to local climate conditions will be applied for selected Nordic sub-regions, going from 25 km to ~1 km horizontal resolution. The Climate Scenarios group asked for input from other groups on which areas should be used /ces/nr/1671

• 19. HARMONIE - numerical weather prediction model 

  of HARMONIE at IMO The current (autumn 2015) set up of HARMONIE is as follows: HARMONIE version 38h1.2 Domain includes 500x480 horizontal grid points, horizontal resolution 2.5 km, see Figure 2. 65 layers in the vertical, top layer at 10 hPa (~30 km a.g.l.) Simulations are performed four times a day Forecasts length 66 hours, time interval of output 1 hour More information on HARMONIE /weather/articles/nr/3232

• 20. CES_D2.4_VMGO

  5 ECHO-G, Germany/Korea T30L19/0.5-2.8°×2.8°L20 6 GFDL-CM2.1, USA 2.0°×2.5°L24/0.3-1.0°×1.0° 7 IPSL-CM4, France 3.75°x2.5°L19/2°x1°L31 8 MIROC3.2 (medres), Japan T42L20/0.5-1.4°×1.4°L44 9 MRI-CGCM2.3.2, Japan T42L30/0.5-2.0°×2.5°L23 Modeling output involved to calculate extreme indices includes gridded daily distributions of surface air temperature maxima and minima and daily /media/ces/CES_D2.4_VMGO.pdf