36 results were found for WA 0821 7001 0763 (FORTRESS) Pintu Baja 230 Curup Selatan Rejang Lebong.

Results:

• 21. askja_minnisblad_ens

  the lower frequency content of the wave, with main frequency around 0.05 Hz. This low frequency was even measured in the southwestern part of Iceland at a roughly 230 km distance. It probably indicates the main mass movement in the landslide. Drawing: Kristín S. Vogfjörð /media/ofanflod/myndasafn/frodleikur/askja_minnisblad_ens.pdf

• 22. Rockslide in Askja, July 21 2014 - Preliminary results of observations

  was even measured in the southwestern part of Iceland at a roughly 230 km distance. It probably indicates the main mass movement in the landslide. Drawing: Kristín S. Vogfjörð. Fig. 16 Figure 16. Thermal image (upper) and photograph (lower) of the rockslide area taken near Víti at the north side of Öskjuvatn. The thermal image was taken with a FLIR P660 infrared camera. Hot patches /avalanches/articles/nr/2929

• 23. 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

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

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

• 25. IPPC-2007-ar4_syr

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

• 26. CES_D2.4_task1

  of the estimated probability distributions of temperature and precipitation variability as a function of time, up to the year 2050, at 120 Nordic locations for temperature and at 230 locations for precipitation. 2 1. Introduction Weather services base their operational definition of climate on past observations. Commonly, a 30-year normal period such as 1961-1990 is used (World /media/ces/CES_D2.4_task1.pdf

• 27. 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

• 28. VI_2021_008

  /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 29. Journal_of_Hydrology_Veijalainen_etal

  The hydrological simulations were performed with the Wa- tershed Simulation and Forecasting System (WSFS) developed and operated in the Finnish Environment Institute (Vehviläinen et al., 2005). The WSFS is used in Finland for operational hydrolog- ical forecasting and flood warnings (www.environment.fi/water- forecast/), regulation planning and research purposes (Vehviläinen and Huttunen, 1997 /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 30. Bárðarbunga 2014 - September events

  /earthquakes-and-volcanism/articles/nr/3001