87 results were found for Bitrue Invite Code QTZLTET englishtivi Bitrue Exchange.

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• 21. Glacier change sessions at this year's Arctic Circle

  regions decreases and spatial fluctuations in the boundary between cold and warm air can increase in amplitude. Cold air can reach far south in exchange for warmer air that flows into the Arctic regions. In this same session, Stefan Rahmstorf from the University of Potsdam talked about the possible slowdown of deepwater formation north and southwest of Iceland, due to increased melting /about-imo/news/glacier-change-sessions-at-this-year-s-arctic-circle-assembly

• 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. CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction

  accounts for approximately 75% and 65% of the nitrogen and phosphorous discharges, respectively. The marine end member is water from the Belt Sea which forms the transition zone between the North Sea and the Baltic Sea and hence displays large variations in salinity and nutrient concentrations. Exchange of water masses between the estuary and the Belt Sea is mainly driven by wind stress and changes /media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf

• 29. Case_A___Horsens_Fjord

  for approximately 75% and 65% of the nitrogen and phosphorous discharges, respectively. The marine end member is water from the Belt Sea which forms the transition zone between the North Sea and the Baltic Sea and hence displays large variations in salinity and nutrient concentrations. Exchange of water masses between the estuary and the Belt Sea is mainly driven by wind stress and changes /media/loftslag/Case_A___Horsens_Fjord.pdf

• 30. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  the advantages of efficient market exchange of private property) or to centralize its management (by governmental officials guided by a long-term understanding of the public interest). By exogenously im- posing new institutions that either centralized all rights in a single owner (or regulator) or established a market to allocate fully specified rights, it was presumed that overexploitation could /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf