12 results were found for WA 0812 2782 5310 RAB Bangun Taman Mini Samping Rumah Terpercaya Girisubo Gunungkidul.

Results:

• 1. VI_2021_008

  investigation into tremor signals in Iceland. In addition to this tremlog to csv converter, which is limited to the IMO’s historical data, a conversion code was created to convert the widely-used seismic data format mini-SEED to RSAM data. This code reads local mini-SEED files, processes 1-minute windows of seismic data to calculate RSAM, and outputs the Tremv standard csv files. This conversion /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 2. VI_2009_006_tt

  than can be expected to originate from the cauldrons, three to four times the wa- ter equivalent of the accumulation of snow over the watershed of the cauldrons. It has been estimated that flow from the cauldrons, in addition to the jökulhlaups, could be 2–5 m3 s 1 at maximum (Vatnaskil, 2005). It is possible that part of the sulfate-rich groundwater from the glacier comes from the cauldrons /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 3. Milly_etal-2008-Stationarity-dead-Science

  6University of Washington, Seattle, WA 98195, USA. 7NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ 08540, USA. *Author for correspondence. E-mail: cmilly@usgs.gov. An uncertain future challenges water planners. Published by AAAS on July 12, 201 1 www.sciencemag.or g Downloaded from 1 FEBRUARY 2008 VOL 319 SCIENCE www.sciencemag.org574 POLICYFORUM combined with opera- tions /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 4. ces_geus_paakitsoq_full_report

  line shows the difference between the years 1980–2000 and 2060–2080. 7 Discussion It was the original idea of this work to use a mini-ensemble of climate model scenario runs to establish a range of future scenarios of surface mass balance of the ice sheet margin at Paakitsôq. However, it turned out that apart from two older time slice experiments where HIRHAM4 was driven from ECHAM4/OPYC3 (cf /media/ces/ces_geus_paakitsoq_full_report.pdf

• 5. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

  their audience. Climatic Change (2012) 112:233–242 DOI 10.1007/s10584-011-0205-7 C. S. Weiler (*) Office for Earth System Studies, Whitman College, Walla Walla, WA 99362, USA e-mail: weiler@whitman.edu J. K. Keller School of Earth and Environmental Sciences, Chapman University, Orange, CA 92866, USA C. Olex The Point, 121 Jewett Street, Newton, MA 02458, USA 1 Introduction Of all the applications /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 6. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 7. IPPC-2007-ar4_syr

  /media/loftslag/IPPC-2007-ar4_syr.pdf

• 8. 2010_017

  m J M5 [C°] -3 obs. [C°] -4 nce 1 re 5. Comp 26); an int temperatu this system y gridded v picion abo -Jökulsá w similar dif han observ h elevation ces the effe months No ly only on high the tem n band wi refore be s onthly tem an Feb Ma .2 -3.1 -3. .3 -4.1 -3. .1 1.0 0.6 arison of m erpolation re is shown atic differe alues, see T ut the qual atershed; b ference wa ations for t gradient fo /media/ces/2010_017.pdf

• 9. VI_arsskyrsla2020

  it possible at a mini- mum cost to provide high level 24/7 services to all sectors in Iceland as well as for the public. Teresía Guðmundsson led these negotiations on the behalf of IMO. She had been appointed the Director General of IMO in 1946, the first female Director of any national meteorological service and still the only female Director of IMO. ÞJÓNUSTA VIÐ ALÞJÓÐAFLUG Teresía Guðmundsson í /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf

• 10. GA_2009_91A_4_Andreassen

  net balances are wellcorrelated and (obviously) best modelled as the sum of bw measured and bs modelled (bs-m2). Thebest obtained correlations of modelled bw (0.86), bs(0.87) and bn (0.94) for 1949–2006, show that themodel could explain 73, 76 and 88% of the variance over this period.From each year we also extracted the day with maximum bw (bwd) and minimum bs (bsd, mini-mum values as bs is negative /media/ces/GA_2009_91A_4_Andreassen.pdf