89 results were found for WA 0812 2782 5310 Jasa Kanopi Model Talang Air Terpercaya Jaten Karanganyardeskripsi.

Results:

• 51. Publications 2010

  and the parameterization of glacial melting and evapotranspiration in applications of the WaSiM hydrological model within Iceland Bergur Einarsson & Sveinbjörn Jónsson 29 pp 2,4 Mb 2010-016 The effect of climate change on runoff from two watersheds in Iceland Bergur Einarsson & Sveinbjörn Jónsson 34 pp 1,5 Mb 2010-012 Development and Implementation of Seismic Early Warning /about-imo/publications/2010/

• 52. Wind-chill table

  Based on the wind-chill temperature index Árni Sigurðsson 26.2.2010 The wind-chill temperature index is based on a human face model, providing an accurate, understandable, and useful formula for calculating the dangers from winter winds and low temperatures. The index /weather/articles/nr/1827

• 53. Staff members

  Staff members Jens E. Kristinsson Job title: Technician of upper-air soundings /about-imo/employees/persona/44/fyrirtaeki/2

• 54. VI_2014_005

  mode ................................................... 14 5 Errors associated with SURFEX .................................................................... 15 6 Statistical correction of model results .............................................................. 19 7 Original and corrected 2-m air temperature .................................................... 22 8 Original and corrected 10-m /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 55. Volcanic gases

  HBr Carbon dioxide (CO2) Carbon dioxide is denser than air and can accumulate in low-lying areas, thereby decreasing the available oxygen in the air, and can thereby cause oxygen deprivation. At extremely high concentrations, CO2 itself can cause harm to health. Sulfur dioxide (SO2) Sulfur dioxide has a strong smell and can irritate the nose, mouth, throat /volcanoes/volcanic-hazards/volcanic-gases/

• 56. HARMONIE - numerical weather prediction model 

  about 1 km to a few km. At IMO the horizontal resolution is 2.5 km. At this resolution it is possible to simulate explicitly some processes that are important for clouds and precipitation, e.g. the vertical movement of air parcels which improves simulations of updrafts and vertical velocity and thus enables the model to simulate larger convective clouds and convective precipitation (rain and snow /weather/articles/nr/3232

• 57. Hock_Regine_CES_2010rs

  in Scandinavia and Iceland • regional estimates • 2 glaciers (Storglaciären, Mårmaglaciären) Study area: Iceland, Scandinavia ~3,000 km2 ice Storglaciären (3.1 km2) Mårmaglaciären (3.9 km2) ~11,000 km2 ice Data Climate data, calibration period Monthly air temperature: ERA-40 reanalysis (0.5°×0.5°), 1958-2001 Monthly precipitation: Precipitation climatology VASClimO, 1951-2000, 0.5°×0.5° (Beck /media/ces/Hock_Regine_CES_2010rs.pdf

• 58. 2010_005_

  of surface air temperature within the 2004–50 period in the SMHI-RCAO, the MetNo-HIRHAM, and the DMI- HIRHAM5, together with the corresponding model orographies. . . . . . . . . . . 27 6 Mean annual surface air temperature in degrees centigrade during the 1961–90 control period, differences in degrees between the control period and the 2021– 50 reference period, and linear trends in degrees per /media/ces/2010_005_.pdf

• 59. Pyroclastic flow

  of the volcano.Because eruption column density is lower than the atmosphere, the column in most cases ascends many kilometres above the volcano. Finally, it spreads out and forms a cloud and the ash coming from the column is dispersed with the wind. However, when the eruption column can't intake enough air it cools down and becomes denser than the surrounding air. When this happens the column collapses /volcanoes/volcanic-hazards/pyroclastic-flow/

• 60. Eriksson_1-Risk-perception

  of the probability of an adverse event and the magnitude of its consequences (Rayner & Cantor, 1987) Subjective risk perception: • Consequentialist perspective - the consequences of a decision alternative determine risk perception (an expected utility model) (e.g., Payne et al. 1993) • The risk-as-feeling hypothesis - both cognitive evaluations of risks and feelings experienced when making /media/loftslag/Eriksson_1-Risk-perception.pdf