The potential of a mobile group blog to support cultural learning among overseas students

We explored the use of mobile social software, in the form of a mobile group blog, to assist cultural learning. The potential of using this technology for cultural adaptation among overseas students was examined as those students adapted to the everyday life of studying abroad. Two pilot studies and a successful field study of a mobile group blog as used by UK overseas students are reported. A further study with prospective overseas students witnessing this ‘moblogging’ in China revealed the advantages of communicating through this technology as a form of peer-supported preparation for cultural adaptation. Potential advantages for learning a second language via this system, were highlighted as communication was interweaved with cultural adaptation and exercised in the blog entries. Given mobile internet, the language experience together with cultural observation impressively supported these students' growing confidence with time, space and imagination

Toward quantifying the increasing role oceanic heat in sea ice loss in the new Arctic

Author Posting. © American Meteorological Society, 2015. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Bulletin of the American Meteorological Society 96 (2015): 2079–2105, doi:10.1175/BAMS-D-13-00177.1.The loss of Arctic sea ice has emerged as a leading signal of global warming. This, together with acknowledged impacts on other components of the Earth system, has led to the term “the new Arctic.” Global coupled climate models predict that ice loss will continue through the twenty-first century, with implications for governance, economics, security, and global weather. A wide range in model projections reflects the complex, highly coupled interactions between the polar atmosphere, ocean, and cryosphere, including teleconnections to lower latitudes. This paper summarizes our present understanding of how heat reaches the ice base from the original sources—inflows of Atlantic and Pacific Water, river discharge, and summer sensible heat and shortwave radiative fluxes at the ocean/ice surface—and speculates on how such processes may change in the new Arctic. The complexity of the coupled Arctic system, and the logistic and technological challenges of working in the Arctic Ocean, require a coordinated interdisciplinary and international program that will not only improve understanding of this critical component of global climate but will also provide opportunities to develop human resources with the skills required to tackle related problems in complex climate systems. We propose a research strategy with components that include 1) improved mapping of the upper- and middepth Arctic Ocean, 2) enhanced quantification of important process, 3) expanded long-term monitoring at key heat-flux locations, and 4) development of numerical capabilities that focus on parameterization of heat-flux mechanisms and their interactions.2016-06-0

Seasonal Movements and Diving of Ringed Seals, Pusa hispida, in the Western Canadian Arctic, 1999–2001 and 2010–11

Satellite-linked time-depth recorders were deployed on 17 ringed seals in early summer in 1999, 2000, and 2010, near the Inuvialuit community of Ulukhaktok, Northwest Territories, Canada. The main objective was to investigate movements and diving behaviour of ringed seals in the Prince Albert Sound (PAS) and eastern Amundsen Gulf (EAG) regions in relation to season, sex, and age-class. Tags performed well on 16 of 17 tagged seals, with average tracking periods of 256 d (SD 69, range: 134 – 352). Adult and subadult ringed seals traveled considerable distances throughout the open water period (mean = 5844 km, range = 1232 – 9473 km), using vast home ranges during this season, shown with 90 Percent Volume Contours (90 PVC) averaging 122 854 km2 for subadults, 76 658 km2 for adult females, and 21 649 km2 for adult males. Overall, adults spent 69.5% of the observed open water days in foraging/resident mode and 22.8% in traveling mode. The majority (75%) of total observed foraging/resident time was spent in PAS and EAG. Eleven of 12 adults made forays outside EAG and PAS to distant areas, including Prince of Wales Strait (7 seals), Viscount Melville Sound (6), Minto Inlet (4), western Amundsen Gulf (4), and six other zones. During open water season, subadults spent 36.8% traveling and 51.4% foraging/ resident, also mainly in EAG and PAS (61%), but they all traveled to distant zones, eight in total. During winter, all tagged adult females, five of seven adult males, and three of four subadults returned to PAS and EAG to occupy winter home ranges that were on average 15% of the size of the open water home range (mean winter ranges = 1299 km2 for adult males, 3599 km2 for adult females, and 30 499 km2 for subadults). The mean size of the winter home ranges varied by as much as a factor of 10 among the three winters examined. Seal movements were most restricted during the winters with extensive fast ice (1999 – 2000 and 2010 – 11) and least restricted during the winter (2000 – 01) when fast ice did not form in EAG. In winter, adult females made more long, deep dives than either adult males or subadults.Des enregistreurs de profondeur temporelle en liaison avec un satellite ont été déployés sur 17 phoques annelés au début des étés 1999, 2000 et 2010 près de la collectivité inuvialuite d’Ulukhaktok, dans les Territoires du Nord-Ouest, au Canada. L’objectif principal consistait à étudier les déplacements et les comportements de plongée des phoques annelés des régions du détroit de Prince-Albert (DPA) et de la partie est du golfe Amundsen (EGA) en fonction de la saison, du sexe et de la classe d’âge. Les étiquettes ont donné des résultats valables dans le cas de 16 des 17 phoques étiquetés, les périodes moyennes de pistage ayant atteint 256 jours (SD 69, étendue : 134 – 352). Les phoques annelés adultes et jeunes adultes parcouraient des distances considérables pendant la période des eaux libres (moyenne = 5 844 km, étendue = 1 232 – 9 473 km), dans de vastes domaines vitaux au cours de la saison. Les pourcentages du volume des contours de 90 (90 PVC) s’établissaient en moyenne à 122 854 km2 pour les jeunes adultes, à 76 658 km2 pour les femelles adultes et à 21 649 km2 pour les mâles adultes. Dans l’ensemble, les adultes ont passé 69,5 % des journées observées en eaux libres en mode d’alimentation et de résidence, et 22,8 % en mode de déplacement. La majorité (75 %) du temps total observé en mode d’alimentation et de résidence était dans le DPA et l’EGA. Onze adultes sur 12 se sont aventurés en dehors du DPA et de l’EGA pour atteindre des endroits éloignés, dont le détroit du Prince-de-Galles (7 phoques), le détroit du Vicomte de Melville (6), l’anse Mintot (4), l’ouest du golfe Amundsen (4) et six autres zones. Pendant la saison des eaux libres, les jeunes adultes ont passé 36,8 % du temps en mode de déplacement et 51,4 % du temps en mode d’alimentation ou de résidence, également principalement dans le DPG et l’EGA (61 %), mais ils se sont tous rendus dans des zones éloignées, huit en tout. Durant l’hiver, toutes les femelles adultes étiquetées, cinq mâles adultes sur sept et trois jeunes adultes sur quatre sont revenus dans le DPA et l’EGA pour occuper des domaines vitaux hivernaux qui correspondaient, en moyenne, à 15 % de la taille du domaine vital en eaux libres (étendues moyennes des domaines hivernaux = 1 299 km2 pour les mâles adultes, 3 599 km2 pour les femelles adultes et 30 499 km2 pour les jeunes adultes). La taille moyenne des domaines vitaux hivernaux a varié en fonction d’un facteur de 10 au cours des trois hivers à l’étude. Le déplacement des phoques était plus restreint pendant les hivers où la glace était rapide (1999-2000 et 2010-2011) et moins restreint pendant l’hiver (2000-2001) où la glace rapide ne s’est pas formée dans l’EGA. L’hiver, les femelles adultes faisaient plus de plongées longues et profondes que les mâles adultes ou les jeunes adultes

Chinese students in a UK business school: hearing the student voice in reflective teaching and learning practice.

This paper presents the outcomes of a study carried out in 2001-2002 with nine postgraduate students from China, enrolled on taught master's programmes in a UK university business school. The aims of the research were to explore the development of the students' orientations to learning during their year of study in the UK, and to explore how the researcher's interactions with the study group contributed to her professional reflections and influenced her academic practice. The main conclusions of the project were that participants' underlying approaches to learning did not change substantially over the year, owing to the culturally implicit nature of UK academic conventions and that they experienced high levels of emotional isolation and loneliness, which affected their academic confidence

The role of eddies on particle flux in the Canada Basin of the Arctic Ocean

AbstractMoorings with sequential sediment traps to study downward sediment flux in the Canada Basin of the Arctic Ocean were maintained in 3350m of water year-round between September 1990 and July 1994. Sediment was collected nominally at 600-m depth and instruments measuring current, temperature, salinity and pressure were placed at several levels between 45 and 1515m. Total dry weight particle fluxes were low (4.2, 2.1, and 8.2gm−2a−1) compared to those found in other world ocean basins. Particle flux varied greatly intra-annually. There were peaks during each summer, with differing seasonal timing and particle composition suggesting a correlation with inter-annual differences in summertime ice clearance. In winter, the particle flux was higher if the ice of the preceding summer was light. Enhanced primary production in summers with wider ice-free seas is a possible explanation, but inconsistent with the high lithogenic (LITH) content of most samples: A significant fraction of the particulate organic carbon (POC) content is refractory carbon. Another possibility is that the south-easterly wind pushing ice to the north-west in summers of reduced ice drives the Mackenzie River plume, laden with lithogenic sediment, behind it and out to the mooring site. There is also another factor in play: Peaks in particle flux frequently coincided with eddies, mesoscale circulation features with strongest current well below the surface. The highest measured flux occurred in the winter of 1994, synchronous with a baroclinic eddy which enveloped the mooring for 60 days while rotating cyclonically and moving slowly north-westward. Particles trapped at this time had high LITH and low POC contents, a relatively high molar ratio of biogenic silica to POC and appreciable chlorophyll a and phaeophytin pigments. Subsequent trap intervals coincided with the passage of a deeper anti-cyclonic eddy, also on a north-westward trajectory, which deposited material of different composition. These observations demonstrate that an understanding of the lateral transport of sediment by energetic physical phenomena is critical to the insightful interpretation of the particle flux measured with sediment traps at sites remote from the coast in the southern Canada Basin