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We present a workflow to track icebergs in proglacial fjords using oblique time-lapse photos and the Lucas-Kanade optical flow algorithm. We employ the workflow at LeConte Bay, Alaska, where we ran five time-lapse cameras between April 2016 and September 2017, capturing more than 400 000 photos at frame rates of 0.5–4.0 min−1. Hourly to daily average velocity fields in map coordinates illustrate dynamic currents in the bay, with dominant downfjord velocities (exceeding 0.5 m s−1 intermittently) and several eddies. Comparisons with simultaneous Acoustic Doppler Current Profiler (ADCP) measurements yield best agreement for the uppermost ADCP levels (~ 12 m and above), in line with prevalent small icebergs that trace near-surface currents. Tracking results from multiple cameras compare favorably, although cameras with lower frame rates (0.5 min−1) tend to underestimate high flow speeds. Tests to determine requisite temporal and spatial image resolution confirm the importance of high image frame rates, while spatial resolution is of secondary importance. Application of our procedure to other fjords will be successful if iceberg concentrations are high enough and if the camera frame rates are sufficiently rapid (at least 1 min−1 for conditions similar to LeConte Bay).
Submarine melting at the ice–ocean interface is a significant term in the mass balance of marine-terminating outlet glaciers. However, obtaining direct measurements of the submarine melt rate, or the ocean heat transport towards the glacier that drives this melting, has been difficult due to the scarcity of observations, as well as the complexity of oceanic flows. Here we present a method that uses synoptic velocity and temperature profiles, but accounts for the dominant mode of velocity variability, to obtain representative heat transport estimates. We apply this method to the Sermilik Fjord–Helheim Glacier system in southeastern Greenland. Using lowered acoustic Doppler current profiler (LADCP) and hydrographic data collected in summer 2009, we find a mean heat transport towards the glacier of 29 × 109W, implying a submarine melt rate at the glacier face of 650 ma–1. The resulting adjusted velocity profile is indicative of a multilayer residual circulation, where the meltwater mixture flows out of the fjord at the surface and at the stratification maximum.
Interaction of Greenland’s marine-terminating glaciers with the ocean has emerged as a key term in the ice-sheet mass balance and a plausible trigger for their recent acceleration. Our knowledge of the dynamics, however, is limited by scarcity of ocean measurements at the glacier/ocean boundary. Here data collected near six marine-terminating glaciers (79 North, Kangerdlugssuaq, Helheim and Petermann glaciers, Jakobshavn Isbræ, and the combined Sermeq Kujatdleq and Akangnardleq) are compared to investigate the water masses and the circulation at the ice/ocean boundary. Polar Water, of Arctic origin, and Atlantic Water, from the subtropical North Atlantic, are found near all the glaciers. Property analysis indicates melting by Atlantic Water (AW; found at the grounding line depth near all the glaciers) and the influence of subglacial discharge at depth in summer. AW temperatures near the glaciers range from 4.5˚C in the southeast, to 0.16˚C in northwest Greenland, consistent with the distance from the subtropical North Atlantic and cooling across the continental shelf. A review of its offshore variability suggests that AW temperature changes in the fjords will be largest in southern and smallest in northwest Greenland, consistent with the regional distribution of the recent glacier acceleration.
Icebergs calved from tidewater glaciers represent about one third to one half of the freshwater flux from the Greenland ice sheet to the surrounding ocean. Using multiple satellite datasets, we quantify the first fjord-wide distributions of iceberg sizes and characteristics for three fjords with distinct hydrography and geometry: Sermilik Fjord, Rink Isbræ Fjord and Kangerlussuup Sermia Fjord. We estimate average total iceberg volumes in summer in the three fjords to be 6.4 ± 1.5, 1.7 ± 0.40 and 0.16 ± 0.09 km3, respectively. Iceberg properties are influenced by glacier calving style and grounding line depth, with variations in size distribution represented by exponents of power law distributions that are −1.95 ± 0.06, −1.87 ± 0.05 and −1.62 ± 0.04, respectively. The underwater surface area of icebergs exceeds the subsurface area of glacial termini by at least one order of magnitude in all three fjords, underscoring the need to include iceberg melt in fjord freshwater budgets. Indeed, in Sermilik Fjord, we calculate summertime freshwater flux from iceberg melt of 620 m3 s−1 (±140 m3 s−1), similar in magnitude to subglacial discharge. The method developed here can be extended across Greenland to assess relationships between glacier calving, iceberg discharge and freshwater production.
This volume explores the diverse ways in which the Book of Psalms profoundly influenced medieval English literature and culture, through a series of connected overviews and special case studies. A number of recent studies have highlighted the Psalter's reception in Early Modern English (and wider European culture), while three monographs by contributors to this volume offer focused studies of the Psalter in individual periods of medieval English literature: Jane Toswell's The Anglo-Saxon Psalter, Annie Sutherland's English Psalms in the Middle Ages: 1300–1450and Michael P. Kuczynski's Prophetic Song: The Psalms as Moral Discourse in Late Medieval England. But as yet no single study has sought to offer a comprehensive survey of English responses to the Book of Psalms from the conversion of the Anglo-Saxons to the cusp of the Reformation. By bringing work by experts on both Old and Middle English literature into dialogue, this volume breaks down the traditional disciplinary binaries of pre- and post-Conquest English, late medieval and Early Modern, as well as emphasizing the complex and fascinating relationship between Latin and the vernacular languages of England. In order to encourage the reader to make connections both across and within these various periods and languages, the book is arranged thematically rather than chronologically, with three sections designed to offer a variety of perspectives on the Psalms and medieval English literature.
Section I (Translation) focuses on the development of English psalm translation from its beginnings in Old English interlinear glosses in Latin psalters through the multilingual psalters of the Anglo-Norman era to the stand-alone vernacular psalters of the fourteenth and fifteenth centuries. Concentrating on the Psalter as a book, this section charts the emergence of English as a scriptural language in the medieval period.
Section II (Adaptation) considers how medieval English prose and verse writers draw on the Psalms as a source of literary inspiration. Demonstrating how the Psalter could be adapted and redeployed within the context of medieval worship and prayer, it begins with a discussion of the first adaptation of the entire Psalter into English verse, before turning to a consideration of the development of the abbreviated psalter tradition. This section also addresses the wider influence of psalmic language and imagery on Old English praise and lament poetry, and on Middle English alliterative verse.
The Book of Psalms had a profound impact on English literature from the Anglo-Saxon to the late medieval period. This collection examines the various ways in which they shaped medieval English thoughtand contributed to the emergence of an English literary canon. It brings into dialogue experts on both Old and Middle English literature, thus breaking down the traditional disciplinary binaries of both pre- and post-Conquest English and late medieval and Early Modern, as well as emphasizing the complex and fascinating relationship between Latin and the vernacular languages of England. Its three main themes, translation, adaptation and voice, enable a rich variety of perspectives on the Psalms and medieval English literature to emerge.
Tamara Atkin is Senior Lecturer in Late Medieval and Early Renaissance Literature at Queen Mary University of London; Francis Leneghan is Associate Professor of Old English at The University of Oxford and a Fellow of St Cross College, Oxford.
Contributors: Daniel Anlezark, Mark Faulkner, Vincent Gillespie, Michael P. Kuczynski, David Lawton, Francis Leneghan, Jane Roberts, Mike Rodman Jones, Elizabeth Solopova, Lynn Staley, AnnieSutherland, Jane Toswell, Katherine Zieman.
This article reports on a case study of a decade-long organizing forms response to the need for groundbreaking innovation while maintaining existing operational performance – the explore–exploit conundrum. Employing ‘grounded research,’ data were collected on the experiences of the Asia-Pacific arm of a multinational professional service firm’s key decision-makers, innovators and entrepreneurs. The findings reveal a three-tiered organizing forms response to the explore–exploit paradox, characterized by a novel combination of heavy exploitation-driven actions alongside deep exploration projects. This case suggests that one successful approach to delivering on both explore and exploit focuses on a productive tension that emerges by enacting innovative organizing forms with contextual awareness. This productive tension was sufficiently powerful to impel individuals to innovate, but also sufficiently contained to avoid interfering with commercial outcomes. An explore–exploit framework conceptualizes organizational changes incorporating complexity and contradiction, without the implicit emphasis on removing or denying the existing tension.