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62 results were found for n 출장안마〔010.4889.4785〕리코건전마사지㙖리코남성전용閛리코딥티슈㴜리코딥티슈출장🗯unanswered/.


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  • 1. Isskyrsla_20100116

    Reykjavík 16. janúar 2010. Til: Veðurstofu Íslands. Frá: Landhelgisgæslu Íslands. Efni: Hafískönnun 16. janúar 2010. Laugardaginn 16. janúar 2010 fór þyrla landhelgisgæslunar TF-EIR í gæslu og ískönnunarflug. Var flogið norður Húnaflóann og fyrir vestfirðina. Einn stakur ísjaki sást í Húnaflóanum á stað : 66°12,7‘N – 21°16,3‘V Komið var að ísröndinni út af Húnaflóa og henni fylgt til vesturs um /media/hafis/skyrslur_lhg/Isskyrsla_20100116_rett.pdf
  • 2. Earthquakes last 48 hours

    9.9 km N of Eldey 2.123.01 02:08:14Check.9.5 km N of Eldey 2.123.01 02:08:1390.09.4 km NNW of Eldey 2.223.01 02:07:57Check.9.9 km N of Eldey 2.623.01 00:56:14Check.9.3 km N of Eldey 2.723.01 00:54:4452.5322.4 km W of Eldeyjarboði 2.322.01 22:34:20Check.19.7 km SW of Húsafell 2.022.01 21:45:54Check.11.4 km N of Eldey 2.122.01 20:18:47Check.9.8 km N /m/earthquakes/latest
  • 3. Guidelines2-for-rapporteurs

    ). This can be helpful with respect to finding a common structure in presenting as well in session reporting (for which angles mentioned in the opening session statements of the Workshop participants can provide checkpoints).” Session rapporteur allocation M o n d a y 2 9 . 8 Y u a n g Z h e n g A t h a n a s i o s V o t s i s E i v i n d J u n k e r M i c h a e l L a i h o H e c to r /media/loftslag/Guidelines2-for-rapporteurs.pdf
  • 4. Isskyrsla_06Jan_2010

    lágu frá aðal ísnum og náðum að meta þéttleikann þar. Ekki sáust neinir borgarísjakar né stakir ísjakar í þessu flugi. Aðalrönd íssins lá í gegnum eftirtalda punkta (tekið með radar). Að sjá var ísinn samfrosta 10/10 1. 66°13,7‘N – 025°35,7‘V 2. 66°24,0‘N – 024°26.0‘V 3. 66°50,1‘N – 023°44,1‘V 4. 67°03,1‘N – 023°31,0‘V 5. 67°00,7‘N – 023°11,3‘V 6. 66°58,7‘N – 022°39,7‘V 7. 66°55,8‘N – 022°23,5‘V /media/hafis/skyrslur_lhg/Isskyrsla_06Jan_2010.pdf
  • 5. Observations - Central - Overview stations

    - Stjórnarsandur | Kolka | Kárahnjúkar | Laufbali | Möðrudalur | Sandbúðir | Svartárkot | Sáta | Tindfjöll | Upptyppingar | Vatnsfell | Veiðivatnahraun Mon 24.01 13 GMT Brúarjökull B10 Observation N/A Búrfell Observation N/A Fagurhólsmýri 2.4° WNW 8 Max wind : 8 / 11 Hallormsstaðaháls -3.3° S 4 Max wind : 4 / 8 Hveravellir -3.5° S 8 Max wind : 10 /m/observations/areas
  • 6. CES_BioFuels_Flyer_new

    ) and changing climate (CC:CC) 1. Current climate (CU) - varying thinning regimes (0%, 15%, 30%,45%) 2. Changing climate (CC) - varying thinning regimes (0%, 15%, 30%,45%) 3. Current (CU) & changing climate (CC) - current thinning regime 4. Current (CU) & changing climate (CC) - changed thinning regimes C l i m a t e s c e n a r i o s M ea s u r e m en t s o f c l i m a t e p /media/ces/CES_BioFuels_Flyer_new.pdf
  • 7. Largest earthquakes during the last 48 hours

    Largest earthquakes during the last 48 hours | Largest | Icelandic Meteorological office Largest earthquakes during the last 48 hours SizeTimeQualityLocation 2.722.01 19:21:45Check.2.0 km NE of Krýsuvík 2.623.01 00:56:14Check.9.3 km N of Eldey 2.522.01 19:02:58Check.9.7 km N of Eldey 2.422.01 18:50 /m/earthquakes/largest
  • 8. Group5-Stakeholders_involvement

    /EPP 2 Stakeholders analysis 26 August 2011 PM/YZ/EPP 3 Stake h o l d e r s P u b l i c / p r i v at e P o w e r l e v e l (“ n u i s an ce” ca p a c i t y ) O r i e n tat i o n H or s t e n s m uni c ipal i t y ( c o m pe t e n t a u t h ori t y ) P u b l i c S t ron g Go v ernanc e N eighbour mun i c i p ali t y P u b l i c S t ron g Go v ernanc e Poli c y /media/loftslag/Group5-Stakeholders_involvement.pdf
  • 9. Sea ice in June 2010

    IMO received five observations on sea ice this month. On the 12th and 14th, ships observed an ice strip at 66°42'N and 24°15' W up to 66°59'N and 22°24'W. On the 14th an observation was also received from the weather station „Hraun á Skaga“ on an iceberg 10-11 nm northwest of Skagatá. On the 22nd an ice strip was observed at 66°49'N /sea-ice/monthly/2010/nr/2341
  • 10. Benestad_Rasmus_CES_2010

    An analysis of simulated and observed storm characteristics - Can we expect a change in the future? R.E. Benestad, CES, June 01 2010 Number of cyclones: RCM analysis CCI (Benestad & Chen, 2006) righttoleftmark No change in storm frequency? RCM: N corresponds |v| too high ...or simulated wind speeds? •CCI •triangulation Method: storm characteristics RCM: storms too small too strong. Gradient /media/ces/Benestad_Rasmus_CES_2010.pdf

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