38 results were found for WA 0821 7001 0763 (FORTRESS) Pintu Baja 240 Tomosiga Intan Jaya.

Results:

• 31. CES_D2.4_task1

  VAERNES NO +63:30:00 +10:53:24 12 TP 1053 RENA - HAUGEDALEN NO +61:09:33 +11:26:33 240 TP 1054 KJOBLI I SNAASA NO +64:09:36 +12:28:12 195 TP 1055 ORLAND NO +63:42:01 +09:36:05 10 TP 1056 SKROVA FYR NO +68:09:01 +14:39:02 11 T 1057 BARDUFOSS NO +69:03:32 +18:32:25 76 /media/ces/CES_D2.4_task1.pdf

• 32. Hare-2011-ParticipatoryModelling

  ea th , th e m et ho d u se d at th is st ag e fo r th es e st ak eh o ld er typ es is sp ec i
  ed .Sh oul d ther e be tw o o r mor e model sbein g develope d in th e process ,the n th e typ e o fmode lt o whic h th e metho d wa s applie d is show n in parentheses .O T re fe rs to th e co m po si tio n o ft he o rg an iz in g te am . Fo r o rg an iz in g te am in vo lve m en t in di ffe re n t pa rt /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 33. VI_2014_005

  reanalysis project is 37h1.2. The simulations were run on the c2a supercomputer at the European Centre for Medium Range Weather Forecasts (ECMWF). The model domain is the same as the one used for the IMO operational forecast runs (DOMAIN=ICELAND)2, with 300 240 horizontal grid points, and a horizontal grid-point spacing of about 2.5 km in both directions. HARMONIE uses a terrain-following sigma /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 34. VI_2015_006

  Meteorological Office (IMO) between 2011 and 2014. The model do- main is also the same as for the IMO operational runs, with 300 240 horizontal grid points cov- ering the whole of Iceland and parts of the surrounding ocean, and with a horizontal grid-point spacing of about 2.5 km in both directions. The model is run with the standard 65 vertical levels, and with a non-hydrostatic dynamic core /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 35. 2010_003rs

  A suite of possible mechanisms are calculated for each event based on polarities and spectral amplitudes. Through the joint interpretation of fault mechanisms with the event distribution defining the fault, the slip direction on the fault plane can be inferred. Using this kind of mapping, about 240 faults, fault segments and small clusters, which were active in year 2000, have been mapped during /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 36. VI_arsskyrsla2020

  /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf

• 37. Reykholt-abstracts

  /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 38. ces-oslo2010_proceedings

  /media/ces/ces-oslo2010_proceedings.pdf