82 results were found for mexc exchange Referral Code 15LQV.

Results:

• 21. NONAM_1st_workshop_summary_v3

  was to strengthen links and exchange information among Nordic researchers and practitioners in adaptive management related to adaptation to climate change. The workshop focused on three topics: (i) What is the difference between adaptation and adaptive management; (ii) Participatory planning processes – group model building; and (iii) Uncertainty and risk assessment. The workshop was organised /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 22. Early work and an overview of measurements

  Nansen both wrote interesting papers on the subject after Thoroddsen died. Their conclusions were similar to Thoroddsen's. These supported the work of the Danish scientist Speerschneider, the compiler of sources on ice off the coast of Denmark from AD 700 onwards. He concluded that no significant long-term changes had occured during this period. Thoroddsen did exchange views with the differently /climatology/articles/nr/1138

• 23. Early work and an overview of measurements

  Nansen both wrote interesting papers on the subject after Thoroddsen died. Their conclusions were similar to Thoroddsen's. These supported the work of the Danish scientist Speerschneider, the compiler of sources on ice off the coast of Denmark from AD 700 onwards. He concluded that no significant long-term changes had occured during this period. Thoroddsen did exchange views with the differently /climatology/articles/nr/1138/

• 24. VI_2009_006_tt

  Special thanks go to Gwenn E. Flowers at the Simon Fraser University in Vancou- ver for providing me with her Matlab code for the coupled sheet–conduit model, for her comments and assistance with model calibration and discussions of model results. I thank Finnur Pálsson and Helgi Björnsson at the Institute of Earth Sciences at the University of Iceland for providing profiles of the subglacial flood /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 25. ces_geus_paakitsoq_full_report

  for melt (Qm) is calculated as follows: Qm = (1 − α)Sin + C0 + C1Ta (2) Where α is the albedo for the surface (three fixed albedo values are applied: snow = 0.8, firn = 0.55 and ice = 0.42), Ta is in ◦C and C0 +C1Ta is the sum of the longwave radiation balance and the turbulent exchange (Oerlemans, 2001). C1 is set to 10 Wm−2 K−1 (Oerlemans, 2001) and C0 is tuned to −45 Wm−2 K−1. Accumulation equals /media/ces/ces_geus_paakitsoq_full_report.pdf

• 26. Moellenkampetal_etal-2010

  team-member objectives, interactions, conflicts, and collective choices shape the intervention process and impact the participatory processes design, as well as how we sought to code and interpret this data relative to the negotiation theory. Data and Interpretation For both intervention cases, a dedicated formal evaluation was conducted by an external observer who attended some design meetings /media/loftslag/Moellenkampetal_etal-2010.pdf

• 27. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  variations, gas exchange measurements and environmental information. While I am still in the infant stages of my dissertation, my plan is to first, understand physiological growth from changes in the environment through diameter changes. Then, I will use this understanding to interpret growth to seasons with drought, and from laboratory experiments, to elevated levels of CO2. Topics /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 28. Bárðarbunga 2014 - October events

  Holuhraun lava field Excerpt from a satellite image 7 October 2014 for the IsViews project at LMU which Fjarkönnun is part of. This Quicklook radar image from TerraSAR-X, irrespective of weather and visibility, shows the outlines of the new lava in exceptionally high detail (see full image) as they were two days ago. Referral: (c) DLR/ Fjarkönnun ehf./IsViews 10/2014. 9 October /earthquakes-and-volcanism/articles/nr/3011

• 29. Bardarbunga-2014_October-events

  the outlines of the new lava in exceptionally high detail (see full image) as they were two days ago. Referral: (c) DLR/ Fjarkönnun ehf./IsViews 10/2014. 9 October 2014 07:00 - from geoscientist on duty Seismic activity at Bárðarbunga is similar as before. Two earthquakes over M4 occurred the last 12 hours at the northern rim of the caldera: 18:49 M4.6 (8 Oct.) 04:37 ca. M5 The subsidence /media/jar/Bardarbunga-2014_October-events.pdf

• 30. Bárðarbunga 2014 - October events

  Holuhraun lava field Excerpt from a satellite image 7 October 2014 for the IsViews project at LMU which Fjarkönnun is part of. This Quicklook radar image from TerraSAR-X, irrespective of weather and visibility, shows the outlines of the new lava in exceptionally high detail (see full image) as they were two days ago. Referral: (c) DLR/ Fjarkönnun ehf./IsViews 10/2014. 9 October /earthquakes-and-volcanism/articles/nr/3011/