26 results were found for 하이로미로미▥문의카톡 gttg5▥㍓하이로미로미출장椢하이마사지賙하이마사지샵䭂하이마사지업소🤸🏽‍♂️longitude/.

Results:

• 11. Climate Report

  /longitude box extending from 10–30W and 60–70N) revealed that the model ensemble average exhibited considerable warming in the last decades of the 20th century and into the 21st, but the warming rate was half of the warming rate that actually occurred. If the CMIP5 ensemble average warming is used as an indicator of the forced (anthropogenic) warming trend, then about half of the recent observed /climatology/iceland/climate-report

• 12. Climate Report

  /longitude box extending from 10–30W and 60–70N) revealed that the model ensemble average exhibited considerable warming in the last decades of the 20th century and into the 21st, but the warming rate was half of the warming rate that actually occurred. If the CMIP5 ensemble average warming is used as an indicator of the forced (anthropogenic) warming trend, then about half of the recent observed /climatology/iceland/climate-report/

• 13. VI_2015_005

  with different MSLP modes, are discussed in Section 7. 2 Data The basis for this study are ERA-40 and ERA-Interim gridded reanalyses produced by the Eu- ropean Centre for Medium-Range Weather Forecasts (ECMWF) (Berrisford et al., 2009; Sim- mons, Uppala, Dee, & Kobayashi, 2006; Uppala et al., 2005). All reanalysis fields are available at a uniform 1-degree resolution in latitude and longitude. Over /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 14. 2010_012rs

  /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 15. CES_D2.4_task1

  --------------------------------------------------------------------------- STAID = ECA&D STATION IDENTIFIER NAME =STATION NAME CN = COUNTRY CODE HGT = HEIGHT ABOVE SEA LEVEL T = TABLES AVAILABLE FOR TEMPERATURE P = TABLES AVAILABLE FOR PRECIPITATION --------------------------------------------------------------------------- STAID NAME CN LATITUDE LONGITUDE HGT 1 VAEXJOE /media/ces/CES_D2.4_task1.pdf

• 16. 2010_003rs

  /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 17. VI_2014_005

  temperature, and 10-m horizontal wind. Initial and boundary conditions for the model simulations discussed here are provided by ECMWF operational analyses (BDSTRATEGY=simulate_operational), with a boundary data interval of three hours (BDINT=3), and a horizontal resolution of 0.125 degrees in longitude and latitude (Andersson and Thépaut, 2008; Bechtold et al., 2008). The lateral boundaries /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 18. Journal_of_Hydrology_Veijalainen_etal

  in the reference period and the larger the ratio between spring and other floods, the more the floods on average decreased. Other variables that were correlated with the results included lat- itude, longitude, lake percentage, size of the watershed, average winter temperature and average maximum snow water equivalent (SWE). The coefficient of multiple correlation R for all these vari- ables was 0.88 in 2070 /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 19. VI_2009_012

  A is similar to the present velocity-attenuation formula used at IMO to estimate local magnitude ML, which is given by: 8.4)(log1.2)(maxlog 1010 −+⋅−= Mrvelocity Date (yyyymmdd) Origin time (hhmmss.ms) Latitude (˚N) Longitude (˚W) MLw (M0 SIL) Mw (M0SIL) MLw (M0CMT) Mw (M0CMT) 20000621 005146.985 63.973 20.711 6.6*) 6.6 6.5 6.4 20000617 154040.998 63.973 20.367 6.4*) 6.2 6.5 6.5 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 20. VI_2009_002rs

  /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_002rs.pdf