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  • 51. Climatological data

    (measured at 9 am) month/year rx_dag1 date of 24-hr maximum precipitation month/year p average sea level pressure nh mean cloud cover, oktas sun number of bright sunshine hours f mean wind speed (m/s) Longer series for selected stations Reykjavík from 1931 Stykkishólmur from 1823 Akureyri from 1931 Grímsstaðir from 1931 Raufarhöfn from 1931 Teigarhorn from 1873 /climatology/data/
  • 52. Glossary

    We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208
  • 53. Glossary

    We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208/
  • 54. Bio Energy

    The International Forestry Review 12(5), p 28. Alam, A., Kilpeläinen, A. and Kellomäki, S. (2010). Forest biomass for energy production ? Potentials, management and risks under climate change. Conference on Future Climate and Renewable Energy: Impacts, Risks and Adaptation, 31.5. ? 2.6.2010, Oslo, Norway. Conference Proceedings pp. 50-51. Kellomäki, S. (2007). In: J. Fenger (Ed.) Impacts of Climate Change /ces/publications/nr/1939
  • 55. Milly_etal-2008-Stationarity-dead-Science

    appears to be driving a poleward expansion of the subtropical dry zone (8), thereby reducing runoff in some regions. Together, circulatory and thermodynamic responses largely explain the picture of regional gainers and losers of sustainable freshwater availability that has emerged from climate models (see figure, p. 574). Why now? That anthropogenic climate change affects the water cycle (9 /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf
  • 56. Publications

    and cold. CE flyer 4. [Flyer] Hisdal, H., Kuusisto, E., Barthelmie, R., Lizuma, L., Lindström, G., Jónsson, P., Kriauciuniene, J., & Reihan, A. (2006). Climate and Energy 2003-2006, Statistical Analysis. CE flyer 5. [Flyer] Rummukainen, M., Christensen, J. H., Ólafsson, H., Jylhä, K., & Førland, E. (2006). Climate and Energy 2003-2006, Climate Scenarios. CE flyer 6. [Flyer] Fidje /climatology/research/ce/publications/
  • 57. VI_2015_009

    by rescaling a dimensionless regional flood frequency distribution or growth curve, qR(D;T ), com- mon to all sites of the homogeneous region, with the so-called index flood, µi(D), of the target site: bQi(D;T ) = µi(D)qR(D;T ); (1) where bQi(D;T ) is the estimated flood quantile, i.e. the T -year flood peak discharge averaged over duration D, at site i. The regional growth curve, qR(D;T /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
  • 58. High resolution precipitation maps for Iceland

    maps for 1971-2000 Daily precipitation maps are available on request and further information on the making of the maps. IMO's contacts for this project are Philippe Crochet and Tómas Jóhannesson. Reference: Crochet, P., T. Jóhannesson, T. Jónsson, O. Sigurðsson, H. Björnsson, F. Pálsson and I. Barstad (2007): Estimating the spatial distribution of precipitation in Iceland using a linear model /weather/articles/nr/1625
  • 59. NONAM_participants

    Participation list Name Email Adriaan Perrels adriaan.perrels@fmi.fi Ana Gargallo-Castel gargallo@unizar.es Annika Carlsson annika.carlsson-kanyama@foi.se Ágúst Gunnar Gylfason agust@rls.is Ásta Ósk Hlöðversdóttir aoh3@hi.is Bergur Einarsson bergur@vedur.is Birna Björnsdóttir birna@skipulag.is Emmanuel P. Pagneux emmanuel@vedur.is Esther Hlíðar Jensen esther@vedur.is Gareth James Lloyd gjl /media/vedurstofan/NONAM_participants.pdf
  • 60. Lawrence_Deborah_CES_2010

    ECHAM4/OPYC3 NorClim/HIRHAM 25x25 km 'Empirical Adjustment' to 1 x 1 km 100 150 200 250 300 350 400 450 500 550 600 650 700 750 800 850 900 1 10 100 1000 Return period (years) P e a k d a i l y d i s c h a r g e ( m 3 / s ) 1981-2010 GEV from annual max series 2021-2050 GEV from annual max series 2021 - 2050 Annual maximum series 1981 - 2010 Annual maximum series 1981-2010 200-year flood 2021 /media/ces/Lawrence_Deborah_CES_2010.pdf

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