43 results were found for WA 0859 3970 0884 RAB Pasang Interior Rak TV Untuk Ruangan Kecil WIlayah Klaten.

Results:

• 21. Climate and Modeling Scenarios

  ” (Poster) at at ESF-COST High Level Research Conference “Extreme Environmental Events” in Cambridge, 13.-17. December 2010. Jokinen, P. Several interviews especially related to severe weather, extreme heat and climate change for radio (~10 interviews), TV (one interview) and daily press (dozens) in late July and beginning of August. Jylhä, K. Four interviews by TV channels in Septemer and December /ces/publications/nr/1680

• 22. VAT_newsletter_2018_06

  /media/Eplicanámskeið/VAT_newsletter_2018_06.pdf

• 23. 2013_001_Nawri_et_al

  model setup are typically too large by up to an order of magnitude. This, combined with strong forcing at the model boundaries, results in a systematic spatial bias in low-level wind speed, with too strong winds in coastal regions, and too weak winds in the interior. Figure 5 shows a comparison of average wind speed at 10 mAGL between the WRF model and station measurements. Model data is interpolated /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 24. 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

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

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

• 26. 2010_005_

  scenario, precipitation increased by 10–15% from 1961–90 to 2070–99, and by 5–10% for the lower emitting scenarios (corresponding to approximately 0.5–1% per decade). The CE project also examined RCM results for Iceland based on the HIRHAM model (Haugen and Iversen, 2006). These results showed enhanced warming over the interior of Iceland compared with the coastal zone, and a tendency for enhanced /media/ces/2010_005_.pdf

• 27. IPPC-2007-ar4_syr

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

• 28. VI_2015_006

  are largest. Positive sensible heat fluxes also occur over the interior regions of Vatnajökull and Hofsjökull at around noon on 27 July, due to the cold northeasterly flow over the glaciers (see Figure 10). However, along the edges and on the other icecaps, sensible heat fluxes under clear skies are directed from the atmosphere to the snow. On 3 August, with clear skies, weak winds, and with above freezing /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 29. ces_geus_paakitsoq_full_report

  the interior of the ice sheet is somewhat too dry (Fig. 9b). By average a mean negative precipitation bias of 0.16myr−1 results which equals 43% of the mean from Burgess et al. (2010) (Table 2). 6 Bias Correction and Future Scenario Runs After having specified a number of biases in the RCM output the model runs were repeated with bias-corrected RCM data. To correct the temporal bias of Ta, daily /media/ces/ces_geus_paakitsoq_full_report.pdf

• 30. 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