Measurements in Turbulent Water and Two-Phase Flows by Laser Anemometry

Measurements of the mean and rms values of the longitudinal velocity in a rectangular duct are reported. These results were obtained in a water flow using a laser anemometer. The important design criteria which facilitated the measurements are described and gradient, transit-time, noise and refractive-index corrections are specifically discussed. The results demonstrate the development of a rectangular duct flow and, in particular, reveal that a small lack of symmetry at the duct entrance can readily be identified in the normal- stress results, 37 hydraulic diameters downstream. The possibility of utilizing water droplets in steam and gas bubbles in water to scatter light and thereby to assist laser-anemometer studies of turbulence is discussed. Experimental evidence obtained by the authors and their colleagues is used to support the conclusions

Kuujjua River Arctic Char: Monitoring Stock Trends Using Catches from an Under-Ice Subsistence Fishery, Victoria Island, Northwest Territories, Canada, 1991 – 2009

A standardized, harvest-based monitoring program was conducted during the main under-ice subsistence fishery for Arctic char (Salvelinus alpinus) of the Kuujjua River for 18 winter fishing seasons between 1991 and 2009. The program was a response to the concern of Ulukhaktok residents that Arctic char were becoming fewer in number and smaller in size. Mean harvests averaged 1225 (SD 262) Arctic char annually for 1996–2002 and 568 (SD 274) in 2003–09, or roughly 40% and 20% of the harvest levels estimated for 1971–78 (2900, SD 842) and 1988–92 (2943, SD 1072). There was no statistical relationship between the size of the annual harvest (number of fish), and the corresponding mean annual catch per unit effort (CPUE) value (R2 = 0.0141, p = 0.761). Arctic char were fully recruited to the fishery at age nine, with 82.4% of the sampled catch (n = 3288) ranging between 8 and 12 years and composed almost exclusively (99%) of non-spawning adults. Over the time series, temporal trends were not detected (p > 0.05) in mean annual CPUE (27.3 Arctic char/100 m/24 h, SD 14.15), mean fork length (593 mm, SD 78.1), or mean age (9.9 years, SD 2.0). Annual mortality rate showed a weak, but significant, decreasing trend over the series (R2 = 0.354), and there were no statistical trends in annual values of the Brody growth coefficient (R2 = 0.1337, p = 0.164). Variation in mean annual somatic condition indices was correlated with timing of sea ice clearance in spring (R2 = 0.474, p = 0.002), probably because prey quality, quantity, or both are higher in summers following earlier spring blooms in the marine environment. Together, the absence of temporal trends in CPUE, fork length, and age of the harvested fish and the apparent improvement in survival (lower mortality), suggest that the stock has been stable at the harvest levels observed during the monitoring period. The stock may also be realizing some improved fitness, which is due to changes in environmental productivity and appears to be linked, at least in part, to the timing of spring breakup in eastern Amundsen Gulf.Entre 1991 et 2009, pendant 18 saisons de pêche hivernale, un programme de surveillance standardisé axé sur les récoltes a été réalisé quant à la pêche de subsistance principale d’omble chevalier (Salvelinus alpinus) sur la rivière Kuujjua. Ce programme a été mis en oeuvre à la lumière des inquiétudes exprimées par les résidents d’Ulukhaktok qui affirmaient que le nombre d’ombles chevaliers diminuait, tout comme leur taille. De 1996 à 2002, la récolte moyenne d’ombles chevaliers atteignait 1 225 (SD 262) annuellement, tandis que de 2003 à 2009, la récolte moyenne annuelle s’élevait à 568 (SD de 274), soit environ 40 % et 20 % des récoltes évaluées pour les années 1971 à 1978 (2 900, SD de 842) et les années 1988 à 1992(2 943, SD de 1 072). Il n’existait pas de lien statistique entre la taille de la récolte annuelle (le nombre de poissons) et la valeur de la capture par unité d’effort (CPUE) moyenne annuelle correspondante (R2 = 0,0141, p = 0,761). L’omble chevalier était pleinement recruté à la pêche à l’âge de neuf ans, avec 82,4 % de la capture échantillonnée (n = 3288) variant entre huit et 12 ans, et composée presque exclusivement (99 %) d’adultes non encore reproducteurs. Au fil des séries, aucune tendance temporelle n’a été décelée (p > 0,05) sur le plan de la CPUE moyenne annuelle (27,3 ombles chevaliers/100 m/24 h, SD 14,15), de la longueur moyenne à la fourche (593 mm, SD 78,1) ou de l’âge moyen (9,9 ans, SD 2,0). Le taux de mortalité annuel indiquait une tendance à la baisse à la fois faible mais importante au cours des séries (R2 = 0,354), et il n’y avait pas de tendances statistiques du point de vue des valeurs annuelles du coefficient de croissance de Brody (R2 = 0,1337, p = 0,164). Une corrélation a été établie entre l’écart des indices somatiques annuels moyens et le moment du dégagement de la glace de mer au printemps (R2 = 0,474, p = 0,002), probablement parce que la qualité ou la quantité de proies, ou les deux, est plus élevée au cours des étés qui suivent une prolifération printanière hâtive dans l’environnement marin. Ensemble, l’absence de tendances temporelles relatives à la CPUE, à la longueur à la fourche et à l’âge du poisson récolté et l’amélioration apparente de la survie (mortalité plus faible) suggèrent que le stock était stable aux niveaux de récolte observés pendant la période de surveillance. Par ailleurs, il se pourrait que le stock connaisse une valeur d’adaptation quelque peu améliorée, ce qui est attribuable aux changements caractérisant la productivité environnementale et semble lié, tout au moins en partie, au moment de la débâcle du printemps dans l’est du golfe Amundsen

Dynamics in the deep Canada Basin, Arctic Ocean, inferred by thermistor chain time series

Author Posting. © American Meteorological Society, 2007. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 37 (2007): 1066–1076, doi:10.1175/JPO3032.1.A 50-day time series of high-resolution temperature in the deepest layers of the Canada Basin in the Arctic Ocean indicates that the deep Canada Basin is a dynamically active environment, not the quiet, stable basin often assumed. Vertical motions at the near-inertial (tidal) frequency have amplitudes of 10– 20 m. These vertical displacements are surprisingly large considering the downward near-inertial internal wave energy flux typically observed in the Canada Basin. In addition to motion in the internal-wave frequency band, the measurements indicate distinctive subinertial temperature fluctuations, possibly due to intrusions of new water masses

Ocean circulation and properties in Petermann Fjord, Greenland

The floating ice shelf of Petermann glacier interacts directly with the ocean and is thought to lose at least 80% of its mass through basal melting. Based on three opportunistic ocean surveys in Petermann Fjord we describe the basic oceanography: the circulation at the fjord mouth, the hydrographic structure beneath the ice shelf, the oceanic heat delivered to the under‐ice cavity, and the fate of the resulting melt water. The 1100 m deep fjord is separated from neighboring Hall Basin by a sill between 350 and 450 m deep. Fjord bottom waters are renewed by episodic spillover at the sill of Atlantic water from the Arctic. Glacial melt water appears on the northeast side of the fjord at depths between 200 m and that of the glacier’s grounding line (about 500 m). The fjord circulation is fundamentally three‐dimensional; satellite imagery and geostrophic calculations suggest a cyclonic gyre within the fjord mouth, with outflow on the northeast side. Tidal flows are similar in magnitude to the geostrophic flow. The oceanic heat flux into the fjord appears more than sufficient to account for the observed rate of basal melting. Cold, low‐salinity water originating in the surface layer of Nares Strait in winter intrudes far under the ice. This may limit basal melting to the inland half of the shelf. The melt rate and long‐term stability of Petermann ice shelf may depend on regional sea ice cover and fjord geometry, in addition to the supply of oceanic heat entering the fjord.Keywords: Petermann Fjord\, Greenland, Ocean circulation propertie

Evidence for atmospheric control of sea-ice motion through Nares Strait

Satellite observations of ice motion are combined with model estimates of low‐level winds and surface wind stress to provide evidence for atmospheric control of sea‐ice motion through Nares Strait, between Ellesmere Island and Greenland, during two periods in 2004. The results suggest that ice flux through the strait, and its shutdown through the formation of a landfast ice mass in the strait, can be controlled by wind stress and atmospheric cooling. Analysis of the model results during these two periods also suggest that the intense, low‐level, along‐strait winds are strongly ageostrophic, and may be usefully estimated from pressure differences along the Strait

High heterotrophic CO2 emissions from a Malaysian oil palm plantations during dry-season

Background Tropical peatlands are currently being rapidly cleared and drained for the establishment of oil palm plantations, which threatens their globally significant carbon sequestration capacity. Large-scale land conversion of tropical peatlands is important in the context of greenhouse gas emission factors and sustainable land management. At present, quantification of carbon dioxide losses from tropical peatlands is limited by our understanding of the relative contribution of heterotrophic and autotrophic respiration to net peat surface CO2 emissions. Methods In this study we separated heterotrophic and autotrophic components of peat CO2 losses from two oil palm plantations (one established in ‘2000’ and the other in 1978, then replanted in ‘2006’) using chamber-based emissions sampling along a transect from the rooting to non-rooting zones on a peatland in Selangor, Peninsular Malaysia over the course of three months (June-August, 2014). Collar CO2 measurements were compared with soil temperature and moisture at site and also accompanied by depth profiles assessing peat C and bulk density. Results The soil respiration decreased exponentially with distance from the palm trunks with the sharpest decline found for the plantation with the younger palms. The mean heterotrophic flux was 1244.7 ± SE 149.2 mg m-2h-1 and 663.8 ± SE 102.2 mg m-2h-1 at the 2000 and 2006 plantations, respectively. Autotrophic emissions adjacent to the palm trunks were 944 ± SE 99.7 mg m-2h-1 and 1962 ± SE 246 mg m-2h-1 at the 2000 and 2006 plantations, respectively. Heterotrophic CO2 flux was positively related to peat soil moisture, but not temperature. Total peat C stocks were 60 kg m-2 (down to 1 m depth) and did not vary among plantations of different ages but SOC concentrations declined significantly with depth at both plantations but the decline was sharper in the second generation 2006 plantation. Conclusions The CO2 flux values reported in this study suggest a potential for very high carbon (C) loss from drained tropical peats during the dry season. This is particularly concerning given that more intense dry periods related to climate change are predicted for SE Asia. Taken together, this study highlights the need for careful management of tropical peatlands, and the vulnerability of their carbon storage capability under conditions of drainage

Value diversity and conservation conflict: Lessons from the management of red grouse and hen harriers in England

1. Conflicts between people over wildlife management are damaging, widespread, and notoriously difficult to resolve where people hold different values and worldviews. Cognitive approaches examining steps from human thought to action can help us understand conflict and explore strategies for their management. 2. We focused on the conflict between hunters and conservationists over the management of red grouse (Lagopus lagopus scoticus) and hen harriers (Circus cyaneus) in the English uplands which represents a classic, persistent conflict, where human dimensions are poorly understood. 3. Guided by conceptual frameworks from social and environmental psychology, we conducted a questionnaire‐based study to assess wildlife value orientations of key stakeholders. We quantified attitudes towards hen harriers, grouse shooting, gamekeepers, and raptor conservationists. We also measured support/opposition for harrier management strategies in England and investigated trust in the responsible government authority. 4. We present data from 536 respondents from field sport or nature conservation organizations. Respondents were categorized according to the primary objectives of their affiliated organization: Field sport (i.e., hunters), Non‐raptor, Pro‐raptor, and Pro‐bird (i.e., organizations promoting conservation of birds excluding raptors, raptors specifically, or birds generally). 5. Utilitarian value orientations were prominent among Field sport and Non‐raptor respondents. Most Pro‐raptor and Pro‐bird participants held mutualist value orientations, indicating they did not support shooting or management of wildlife. 6. As suggested by the cognitive hierarchy, we found strong correlations between attitude and support for management options, our proxy for behaviour. 7. Pro‐bird affiliates showed clear preference for less invasive management, and along with Pro‐raptor respondents did not support brood management (removal and later release of eggs/young when harrier density is high). Field sport individuals expressed a degree of support for all management types. Trust in Natural England was limited. 8. Understanding value orientations and attitudes of stakeholders helps explain differences in levels of support for management approaches. Our study highlighted strongly divergent beliefs. Such positions are hard to change. Increasing the level of ecological knowledge alone is unlikely to facilitate conflict management. Instead, conflict management would benefit from combining such knowledge with a focus on relationships, deliberation, and trust in addition to exploring comanagement interventions

The opposite of Dante's hell? The transfer of ideas for social housing at international congresses in the 1850s–1860s

With the advent of industrialization, the question of developing adequate housing for the emergent working classes became more pressing than before. Moreover, the problem of unhygienic houses in industrial cities did not stop at the borders of a particular nation-state; sometimes literally as pandemic diseases spread out 'transnationally'. It is not a coincidence that in the nineteenth century the number of international congresses on hygiene and social topics expanded substantially. However, the historiography about social policy in general and social housing in particular, has often focused on individual cases because of the different pace of industrial and urban development and is thus dominated by national perspectives. In this paper, I elaborate on transnational exchange processes and local adaptations and transformations. I focus on the transfer of the housing model of SOMCO in Mulhouse, (a French house building association) during social international congresses. I examine whether cross-national networking enabled and facilitated the implementation of ideas on the local scale. I will elaborate on the transmission and the local adaptation of the Mulhouse-model in Belgium. Convergences, divergences, and different factors that influenced the local transformations (personal choice, political situation, socioeconomic circumstances) will be taken into accoun