56 results were found for WA 0821 1305 0400 Kontraktor Interior Rumah Ukuran Luas Tanah 60 Murah Duren Sawit Jakarta Timur.

Results:

21. VI_2021_008

Tremv-ALERT: A new early warning system to detect volcanic tremor Bethany Vanderhoof Þórður Karlsson Yesim Cubuk Sabuncu Kristín Jónsdóttir VÍ 2021-008 Skýrsla Tremv-ALERT: A new early warning system to detect volcanic tremor VÍ 2021-008 ISSN 1670- 8261 Skýrsla + 354 522 60 00 vedur @vedur . is Veður st of a Íslands Búst aðaveg ur 7 – 9 108 Reyk j avík Bethany Vanderhoof Þórður Karlsson Yesim /media/vedurstofan-utgafa-2021/VI_2021_008.pdf
22. VI_2015_007

Regional Flood Frequency Analysis: A case study in eastern Iceland Philippe Crochet Tinna Þórarinsdóttir VÍ 2015-007 Report Regional Flood Frequency Analysis: A case study in eastern Iceland VÍ 2015-007 ISSN 1670-8261 Report +354 522 60 00 vedur@vedur.is Veðurstofa Íslands Bústaðavegur 7–9 108 Reykjavík Philippe Crochet, Icelandic Met Office Tinna Þórarinsdóttir, Icelandic Met Office Contents /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf
23. ces_geus_paakitsoq_full_report

Psolid and redistribution of snow is not taken into account. A threshold range of 1 to 2 ◦C is used to distinguish snowfall and rain. Melt-water refreezing is parameterized according to Reeh (1991), using a melt-water retention capacity of 60% of the water equivalent of the snow cover. The glacier mass balance model is designed to operate on large areas. For model input entire grids from RCM output /media/ces/ces_geus_paakitsoq_full_report.pdf
24. Journal_of_Hydrology_Veijalainen_etal

; Jylhä et al., 2008; Räisänen, 2008) and to de- crease snowmelt floods, which are currently the largest floods in most parts of Finland. Significant changes in seasonality of runoff and floods may occur in areas where a large proportion of runoff is from snowmelt (e.g. Lettenmaier et al., 1999; Bates et al., 2008). Finland extends from 70 North with sub-arctic climate to 60 North in the margins /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
25. 2010_016

The effect of climate change on runoff from two watersheds in Iceland Bergur Einarsson Sveinbjörn Jónsson VÍ 2010-016 Report The effect of climate change on runoff from two watersheds in Iceland VÍ 2010-016 ISSN 1670-8261 Report +354 522 60 00 +354 522 60 06 vedur@vedur.is Veðurstofa Íslands Bústaðavegur 9 150 Reykjavík Bergur Einarsson, Icelandic Meteorological Office /media/ces/2010_016.pdf
26. Sea ice in February 2009

northnorthwest of Straumsnesviti and about 60 nm northwest of Barði. Easterly and northeasterly winds were dominant in the Greenland Strait and the sea ice was far off shore the whole month. No dispatches from ships were received from ships and the Coast Guard did not go on an exploration flight /sea-ice/monthly/2009/nr/2324
27. Sea ice in May 2009

during the month. IMO issued information regarding sea ice around mid-month, based on satellite images. The information showed the sea ice was closest to shore about 60 nm northwest of Barði. Easterly winds were predominant in the Greenland Strait /sea-ice/monthly/2009/nr/2327
28. 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 ied .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
29. BIGJ_windrose_2005-2014

Wind rose BIGJ 2005 − 2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 1 2 3 4 5 6 7 Frequency of wind direction (%) Aerodrome Total observations: 1324 Calm: 2.6% Variable winds: 0.23% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 0 45 90 135 180 225 270 315 360 N E S /media/vedur/BIGJ_windrose_2005-2014.pdf
30. GA_2009_91A_4_Andreassen

in southern Norway (Fig.1). The glacier has a total area of 5.4 km2 and rangesin altitude from 1390 to 2090 m a.s.l. The glacierhas been mapped repeatedly, the most recent mapis from 1997. Areas calculated from the 1951 and1997 maps reveal an area reduction of about 0.4km2 in this period (Andreassen 1999). Lengthchange observations reveal a net retreat of about 60 m from 1997 to 2006 (data: NVE; e.g /media/ces/GA_2009_91A_4_Andreassen.pdf