89 results were found for Seydikemer Kasap Çınar Et.

Results:

• 21. Hare_2-participation

  Participatory processes in the real world Conjugation of “to participate” I participate You participate He participates We participate They profit From Arnstein (1969) Matt Hare, Independent Consultant, Mexico hare@gmx.de Participatory Processes in Practice Long-term planning for change 3 “PartizipA“ Local level measures assessment for the Water Framework Directive (Newig et al 2008) 4 /media/loftslag/Hare_2-participation.pdf

• 22. Rolf_Johnsen_(Region_Midt,_Dk)

  distribution, less rainfall in summer and more in winter. The precipitation pattern is expected to have a more dynamic cycle, with longer droughts and more intense rainfalls. As a result, groundwater models predict increases in groundwater levels of up to 2 metres in some areas (Van Roosmalen et al). Sea level will also rise. The precise increase is uncertain but models show increases of up /media/loftslag/Rolf_Johnsen_(Region_Midt,_Dk).pdf

• 23. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

  to the general public remains an ongoing challenge for the climate change research community (Moser andDilling 2004, 2007; Marx et al. 2007; Weart 2008; Leiserowitz 2006; Ward 2008). One area that has not been fully explored within the climate research community is the relationship between psychological personality type (Myers et al. 1998) and preferred communication/learning style. More than 2 million /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

  - over, more detailed documentation of smaller disasters partially explains the earlier mentioned increases. It shows nevertheless that flood and drought problems become more visible and cannot be ignored. Especially since climate change models project more frequent and intense summer droughts across many parts of Europe, particularly in the southern part (Goodess et al. 2007; Fowler et al. 2007 /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 25. Daniell_etal-2010

  (Art. 14). Public participation can be defined as direct participation by nongovernmental actors in decision-making processes (Mostert 2003). Participation is also considered in the literature on adaptive management of natural resources (Gunderson and Holling 2001) and adaptive water governance (Huitema et al. 2009). While the theoretical basis of participation is quite broad, the challenges /media/loftslag/Daniell_etal-2010.pdf

• 26. vanRoosmalen_etal-2009-WRR_2007WR006760

  of climate change on hydrological systems in Europe [e.g., Andre´asson et al., 2004; Arnell, 1999; Caballero et al., 2007; Graham et al., 2007b; Kleinn et al., 2005; Thodsen, 2007]. Generally, the simulated impacts of climate change vary considerably as a result of contrasting climate change signals in northern and southern Europe, e.g., an increase in annual precipitation in the north /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 27. Adalgeirsdottir-etal-tc-5-961-2011

  1Institute of Earth Sciences, University of Iceland, 101 Reykjavík, Iceland 2Danish Meteorological Institute, Lyngbyvej 100, 2100 Copenhagen, Denmark 3Icelandic Meteorological Office, Bústaðavegi 150, 105 Reykjavík, Iceland 4Department of Computer Science, University of Iceland, 107 Reykjavík, Iceland 5CNRS; Université de Toulouse, Laboratoire d’Etudes en Géophysique et Océanographie Spatiales (LEGOS); 14 /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 28. 2010_003rs

  improved the results, it was decided to leave them as they were processed originally, apart from a few minor changes. The main results have partly been published in two reports at Veðurstofan, Rit 21 (Hjaltadóttir and Vogfjörð, 2005) and report 05020 (Hjaltadóttir et al., 2005), but these reports are not nearly as extensive as the following text. The research has also been presented /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 29. New article on glacier changes in

  ), scheduled for publication in 2022. It underscores the importance of long-term research related to climate change.The surface mass balance of the Vatnajökull, Hofsjökull and Langjökull ice caps has been measured systematically in spring and autumn for about 30 years (Helgi Björnsson et al., 2013). The total volume of the main glaciers, as well as Mýrdalsjökull and Drangajökull and some other smaller /about-imo/news/new-article-on-glacier-changes-in-iceland-over-the-past-130-years

• 30. Hock_Regine_CES_2010rs

  et al., 2005) Data Climate data, calibration period Monthly air temperature: ERA-40 reanalysis (0.5°×0.5°), 1958-2001 Monthly precipitation: Precipitation climatology VASClimO, 1951-2000, 0.5°×0.5° (Beck et al., 2005) Elevation-dependent mass balance data for individual glaciers Mass-balance data Data Climate data, calibration period Monthly air temperature: ERA-40 reanalysis /media/ces/Hock_Regine_CES_2010rs.pdf