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[1] To document climate-driven changes in firn stratigraphy and their implications for meltwater flow patterns within firn on the Devon Ice Cap, Nunavut, during the 21st century summer warming, 500 MHz ground-penetrating radar (GPR) surveys were conducted along a 40 km transect in each spring from 2007 to 2012. These linear GPR surveys were supplemented by four 190 m by 100 m GPR grid surveys and 36 firn cores. Increased meltwater percolation and infiltration ice formation associated with high surface melt rates since 2005 modified the firn stratigraphy substantially over a horizontal distance of nearly 30 km. The most dramatic change involved the growth of a thick ice layer within the firn body. This layer grew primarily by upward accretion over an initial widespread ice layer formed during summer 2005. It thickened by between 0.5 and 4.5 m over the study period and filled much of the pore volume in the upper part of the firn, reducing vertical percolation of meltwater into deeper sections of the firn and thus the water storage potential of much of the firn reservoir. Heterogeneous percolation of surface meltwater promoted by rolling topography played an important role in meltwater infiltration and drainage, encouraging lateral flow at the tops of small hills and ponding and refreezing of meltwater beneath surface depressions.

More frequent summer anticyclonic circulation over the Canadian Arctic Archipelago (CAA) between 2007 and 2012 caused more intense and sustained melt of ice caps and glaciers and increased rates of mass loss. To determine the frequency of the occurrence of anticyclonic circulation over the CAA and western Greenland, a self‐organizing map (SOM) was used to classify daily 500 hPa geopotential height (GPH) anomalies calculated from National Centers for Environmental Prediction and the National Center for Atmospheric Research (NCEP/NCAR) Reanalysis 1 (1948–2012) and five Coupled Model Intercomparison Project Phase 5 (CMIP5) models (1950–2025). While the NCEP/NCAR reanalysis indicates that significant summer warming over the CAA is linked to a doubling in the frequency of anticyclonic circulation over the region since 2007, the CMIP5 models were not capable of reproducing the magnitude of the trend in the frequency of anticyclonic circulation over the CAA and western Greenland found in NCEP/NCAR. The variability of the frequency of positive anomalies in summer 500 hPa GPH was found to be related to variability of Arctic sea ice volume/thickness in April, May and June (1979–2012) and to poleward eddy heat flux in June (1979–2012).

ABSTRACT. Evaluation of how accurately snowpack models can capture hydrological processes in firn is critical to determining how well they will simulate future glacier mass-balance changes. Here we compare simulations using the Crocus snowpack model with the evolving firn stratigraphy recorded in 14 cores drilled at four elevations in the accumulation zone of Devon Ice Cap, Canada, during the 2004-12 period of rapid summer warming. Simulations were forced with a combination of surface observations and reanalysis data. Simulations resulted in positive model bias in near-surface density, and negative bias in density at depth compared to observations. Results point to the importance of incorporating heterogeneous percolation in firn in order to improve the representation of meltwater flow, better reproduce observed firn density and temperature profile evolution, and improve simulations of glacier mass balance during periods of climate warming.

R enin-angiotensin system (RAS) is a key component of cardiovascular and renal system homeostasis. RAS activation during development is well described 1 and contributes to organogenesis and growth, especially in the cardiovascular and renal systems. Among RAS components, angiotensin (Ang) II is the major peptide acting during fetal and neonatal life. Both subtypes of Ang receptors are expressed during fetal development 2,3 but have different patterns of expression during the fetal-neonatal transition. In rats, Ang type 2 (AT2) receptors are upregulated in the heart, large vessels, lungs, and kidneys during fetal development and progressively decline after birth, suggesting their contribution to fetal organogenesis. Ang type 1 (AT1) receptors, on the other hand, are detected late in fetal development, increase soon after birth, and are considered to contribute mainly to tissue maturation, growth, and postnatal adaptation. [2][3][4] This switching pattern of Ang receptors suggests that modifications of AT1/AT2 balance play a key role in different developmental stages. A disruption of this balance, depending on the stage of development, may negatively affect cardiovascular and renal homeostasis and contribute to the establishment of cardiovascular diseases.Deleterious perinatal conditions, including preeclampsia, intrauterine growth restriction, and preterm birth can lead to developmental programming of cardiovascular risk factors and diseases. 5,6 Preterm-born individuals in particular, whose numbers are growing in the population because of recent Abstract-Newborn rats exposed to high oxygen (O 2 ), mimicking preterm birth-related neonatal stress, develop later in life cardiac hypertrophy, dysfunction, fibrosis, and activation of the renin-angiotensin system. Cardiac renin-angiotensin system activation in O 2 -exposed adult rats is characterized by an imbalance in angiotensin (Ang) receptors type 1/2 (AT1/2), with prevailing AT1 expression. To study the role of renin-angiotensin system in the developmental programming of cardiac dysfunction, we assessed Ang receptor expression during neonatal high O 2 exposure and whether AT1 receptor blockade prevents cardiac alterations in early adulthood. Sprague-Dawley newborn rats were kept with their mother in 80% O 2 or room air (control) from days 3 to 10 (P3-P10) of life. Losartan or water was administered by gavage from P8 to P10 (n=9/group). Rats were studied at P3 (before O 2 exposure), P5, P10 (end of O 2 ), and P28. Losartan treatment had no impact on growth or kidney development. AT1 and Ang type 2 receptors were upregulated in the left ventricle by high O 2 exposure (P5 and P10), which was prevented by Losartan treatment at P10. Losartan prevented the cardiac AT1/2 imbalance at P28. Losartan decreased cardiac hypertrophy and fibrosis and improved left ventricle fraction of shortening in P28 O 2 -exposed rats, which was associated with decreased oxidation of calcium/calmodulin-dependent protein kinase II, inhibition of the transforming growth factor-β/SMAD3 pathway...

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A catastrophic rain event occurred in early June 2002 during a major drought over the Canadian Prairies. The storm brought record-breaking rainfall and major flooding to many locations in the region. Given the importance of this event, this study's overall objectives are to characterize and to understand the physical nature of the rainstorm better. The event was associated with a major extratropical cyclone which acted in concert with the Great Plains low-level jet to transport a tremendous amount of moisture into the eastern Prairies producing intense diurnal mesoscale convective systems over the region. At the same time, moisture was transported to the western Prairies by a strong easterly low-level jet which produced heavy and long-lived orographic precipitation near the foothills. Several working hypotheses were developed to explain the severity and longevity of the rainstorm; it was found that the Rockies played a central role in the organization and development of the system. Atmospheric features that are critical to the development of an important class of extreme rain events in the Canadian Prairies were also identified. The severity of the June 2002 system is partly a result of the rare co-occurrence of these features during the period. Results from a preliminary analysis show that the atmospheric conditions associated with the extreme background drought enhanced the likelihood of the co-occurrence of these features during spring 2002, hence facilitating the development of the extreme rain event. In return, the tremendous precipitation from the storm alleviated the drought conditions in the southern Prairies.RÉSUMÉ [Traduit par la rédaction] Un événement de pluie catastrophique s'est produit au début de juin 2002 pendant une sécheresse importante dans les Prairies canadiennes. La tempête a produit des chutes de pluie records et des inondations importantes à plusieurs endroits dans la région. Étant donné l'importance de cet événement, les objectifs généraux de la présente étude sont de mieux caractériser et de mieux comprendre la nature physique de la tempête de pluie. L'événement a été causé par une importante dépression extratropicale qui s'est associée au courant-jet à basse altitude des Grandes Plaines pour transporter une énorme quantité d'humidité dans l'est des Prairies et produire d'intenses systèmes convectifs de mésoéchelle diurne dans la région. En même temps, de l'humidité transportée dans l'ouest des Prairies par un fort courant-jet à basse altitude soufflant de l'est a produit d'intenses précipitations orographiques persistantes près des contreforts. Nous avons formulé plusieurs hypothèses de travail pour expliquer l'intensité et la persistance de la tempête de pluie; il ressort que les Rocheuses ont joué un rôle central dans l'organisation et le développement du système.Nous avons aussi identifié les caractéristiques atmosphériques essentielles à la formation d'une catégorie importante d'événements de pluie extrêmes dans les Prairies canadiennes. L'intensité du système de juin 200...

The goal of the Canadian Arctic Weather Science (CAWS) project is to conduct research into the future operational monitoring and forecasting programs of Environment and Climate Change Canada in the Arctic where increased economic and recreational activities are expected with enhanced transportation and search and rescue requirements. Due to cost, remoteness and vast geographical coverage, the future monitoring concept includes a combination of space-based observations, sparse in situ surface measurements, and advanced reference sites. A prototype reference site has been established at Iqaluit, Nunavut (63°45'N, 68°33'W), that includes a Ka-band radar, water vapor lidars (both in-house and commercial versions), multiple Doppler lidars, ceilometers, radiation flux, and precipitation sensors. The scope of the project includes understanding of the polar processes, evaluating new technologies, validation of satellite products, validation of numerical weather prediction systems, development of warning products, and communication of their risk to a variety of users. This contribution will provide an overview of the CAWS project to show some preliminary results and to encourage collaborations.