Download or read book The Role of Sea Ice in Mediating Atmosphere ice ocean Momentum Transfer written by Samuel Dale Brenner and published by . This book was released on 2022 with total page 0 pages. Available in PDF, EPUB and Kindle. Book excerpt: The ongoing loss of Arctic sea ice prompts questions about changes in momentum transfer across the atmosphere-ice-ocean system and potential climate feedback mechanisms, but the role of the ice in mediating that process is not fully understood. To address knowledge gaps about atmosphere-ice-ocean momentum transfer, this study makes use of in situ measurements collected during two recent observational campaigns in the Beaufort Sea: the Marginal Ice Zone (MIZ) program and the Stratified Ocean Dynamics of the Arctic (SODA) program. The research is presented in two parts.Part I develops data processing methods for instrumentation deployed as part of the SODA program while part II uses data from both programs to evaluate controls of sea ice on the ocean surface stress and the associated response in the ocean surface mixed layer (ML). Measurements of upper ocean properties can be challenging in the Arctic Ocean due to environmental conditions, including the need for moored instruments to avoid contact with sea ice. Part I of this work describes methods for developing usable data products from upward-looking Acoustic Doppler Current Profiler (ADCP) measurements on the SODA moorings. This encompasses methods for creating combined data records from vertically-offset ADCPs on the same mooring chain and methods for using ADCPs to estimate surface ML depth and temperature. As ML depth and temperature measurements are not typically possible from subsurface moorings in the Arctic, the approach developed here provides considerable value and could be applied to other extant mooring records to recover information about ML property variability or trends. Building on these measurements, part II considers how sea ice properties, such as concentration and morphology, affect the transfer of momentum from the sea ice to the ocean and the associated upper-ocean dynamics. Ice-ocean drag coefficients, a measure of momentum transfer efficiency, calculated using a force-balance approach from the SODA mooring data show seasonal variations consistent with past observations, but at odds with previous model results.Tests of model parameterizations of drag based on direct observations of under-ice morphology reveal that the model-observation mismatch can be attributed to inaccuracies in empirical translations from bulk geometric properties to detailed geometry statistics, especially under-representation of floe sizes. The mooring measurements further show a seasonal upper-ocean response to surface stress, with minimal energy in ML inertial oscillations under sea ice cover. A simplified momentum budget for the coupled ice-ocean system shows that the seasonality stems from a combination of internal stress in the ice damping the oscillations and seasonal variability in the ocean ML depth. Finally, shipboard measurements from the MIZ program show the evolution of ice-edge-located freshwater front as it reacted to changes in the surface wind stress, raising questions about how sea ice might impact spatial heterogeneity of stress and how that might interact with frontal dynamics. This research shows that boundary layer dynamics and internal ice mechanics both play a role in mediating atmosphere-ice-ocean momentum transfer. The results suggest future trends of more "slippery" ice-ocean boundary layer, and decreasing internal sea ice stress, which could lead to increased sea ice drift speeds and more direct atmosphere-ocean coupling.
Download or read book Understanding Polar Atmosphere ocean sea Ice Momentum Transfer Using Remote Sensing and Modeling Techniques written by Alexander Mchedlishvili and published by . This book was released on 2024 with total page 0 pages. Available in PDF, EPUB and Kindle. Book excerpt: Over the last half a century, the Arctic sea ice extent and volume have been decreasing as a result of the amplified warming taking place in the Arctic. Similarly, the Antarctic summertime sea ice extent maximum has been the lowest in the satellite record for the last three years. As sea ice at both poles is changing in a warming climate, it is necessary to better understand the fundamental processes that determine sea ice properties such as extent, thickness, volume and drift. These processes, namely dynamic and thermodynamic ones, are triggered by the surrounding atmosphere and ocean. The overarching goal of this dissertation is to study dynamic processes while also considering thermodynamic aspects. Chapter 3 delves into the abovementioned dynamic and thermodynamic processes at mesoscale in the study of polynya events and thin sea ice anomalies above Maud Rise in the Antarctic. Chapter 4 looks at parameters that quantify dynamics, specifically at drag coefficients (Cd) that determine the momentum transfer between the atmosphere and sea ice, on a pan-Arctic scale. Finally, Chapter 5 implements the derived estimates of drag from observations into a coupled regional atmosphere-ocean-sea ice model in order to investigate the impact of variable drag on sea ice properties Arctic-wide. The Weddell Sea Polynya (occurring in 1974-1976 and 2016-2017) is an excellent case study in the impact of mesoscale as well as synoptic scale processes on sea ice. My analysis of the events corroborates past studies that identify the Weddell Sea polynya as one that is driven by dynamic as well as thermodynamic processes. In addition, using satellite-borne microwave imaging radiometers, large thin sea ice anomalies have been identified in polynya-free years (2010-2020). Given the reported links between the polynya and different dynamic and thermodynamic ocean and atmosphere processes, our results suggest that when an insufficient amount of these processes are active, a thin sea ice anomaly may emerge instead. The neutral sea ice-atmosphere Cd data-set is the first-ever assessment of drag on both pan- Arctic spatial and sub-yearly temporal scales. Leveraging the high resolution of Ice, Cloud and land Elevation Satellite 2 (IS2), as well as near-coincident Operation IceBridge (OIB) airborne surveys of sea ice topography, it was possible to observe the spatiotemporal evolution of drag from November 2018 to May 2022. My results showed the ice area directly north of the Canadian Archipelago and Greenland to have a Cd consistently above 2.0 × 10-3, while for most of the multiyear ice portion of the Arctic it is typically around ∼1.5 × 10-3. The first-year and young ice portion of the Arctic has a comparatively lower Cd (∼9 × 10-4) with an increase along the marginal ice zone that exceeds 1.5 × 10-3. This dataset was then used to derive a parameterization linking Cd to coincident IS2 sea ice thickness measurements, which was implemented into the regional atmosphere-ocean-sea ice model HIRHAM-NAOSIM. By running the model with and without the implementation, my results showed reasonable albeit small differences between the sea ice properties modelled by the two runs. Using sensitivity studies that varied the coefficients and integration of the Cd parameterization, I was then able to explain the differences observed. The main findings from the model study are that atmospheric and oceanic drag have the opposite effect on both sea ice drift and thickness on a pan-Arctic scale, and that over a period of three years, regardless of the range in drag variability, the impact of drag on sea ice in a coupled model is typically small in magnitude (
Download or read book The Nordic Seas written by Burton G. Hurdle and published by Springer Science & Business Media. This book was released on 2012-12-06 with total page 788 pages. Available in PDF, EPUB and Kindle. Book excerpt: " ... as soon as one has traversed the greater part of the wild sea, one comes upon such a huge quantity of ice that nowhere in the whole world has the like been known." "This ice is of a wonderful nature. It lies at times quite still, as one would expect, with openings or large fjords in it; but sometimes its movement is so strong and rapid as to equal that of a ship running before the wind, and it drifts against the wind as often as with it." Kongespeilet - 1250 A.D. ("The Mirror of Kings") Modern societies require increasing amounts influence on the water mass and on the resulting of scientific information about the environment total environment of the region; therefore, cer tain of its characteristics will necessarily be in whieh they live and work. For the seas this information must describe the air above the sea, included.
Download or read book The Drift of Sea Ice written by Matti Leppäranta and published by Springer Science & Business Media. This book was released on 2011-03-22 with total page 370 pages. Available in PDF, EPUB and Kindle. Book excerpt: The Second Edition of The Drift of Sea Ice presents the fundamental laws of sea ice drift which come from the material properties of sea ice and the basic laws of mechanics. The resulting system of equations is analysed for the general properties of sea ice drift, the free drift model and analytical models for ice drift in the presence of internal friction, and the construction of numerical ice drift models is detailed. This second edition of a much lauded work, unique on this topic in the English language, has been revised, updated and expanded with much new information and outlines recent results, in particular in relation to the climate problem, mathematical modelling and ice engineering applications. The current book presents the theory, observations, mathematical modelling techniques, and applications of sea ice drift science. The theory is presented from the beginning on a graduate student level, so that students and researchers coming from other fields such as physical oceanography, meteorology, physics, engineering, environmental sciences or geography can use the book as a source book or self-study material. First the drift ice material is presented ending with the concept of ‘ice state’ – the relevant properties in sea ice dynamics. Ice kinematics observations are widely presented with the mathematical analysis methods, and thereafter come drift ice rheology – to close the triangle material – kinematics – stress. The momentum equation of sea ice is derived in detail and its general properties are carefully analysed. Then follow two chapters on analytical models: free drift and drift in the presence of internal friction: These are very important tools in understanding the dynamical behaviour of sea ice. The last topical chapter is numerical models, which are the modern tool to solve ice dynamics problem in short term and long term problems. The closing chapter summarises sea ice dynamics applications and the need of sea ice dynamic knowledge and gives some final remarks on the future of this branch of science.
Download or read book Ice in the Ocean written by Peter Wadhams and published by CRC Press. This book was released on 2000-10-31 with total page 376 pages. Available in PDF, EPUB and Kindle. Book excerpt: ICe in the Ocean examines sea ice and icebergs and their role in the global climate system. It is comprehensive textbook suitablefor students, pure and applied researchers, and anyone interested in the polar oceans; the distribution of sea ice; the mechanisms of growth, development and decay; the thermodynamics and dynamics of sea ice; sea ice deformation and ridge-building; the role of marginal ice zones; the characteristics of icebergs; and the part played by sea ice in the climate system and in the transport of pollutants. An extensive reference list and recommendations for further reading and numerous illustrations, and add to the usefulness of the text.
Download or read book Sea Ice written by David N. Thomas and published by John Wiley & Sons. This book was released on 2008-04-15 with total page 419 pages. Available in PDF, EPUB and Kindle. Book excerpt: Sea ice, which covers up to 7% of the planet’s surface, is a major component of the world’s oceans, partly driving ocean circulation and global climate patterns. It provides a habitat for a rich diversity of marine organisms, and is an extremely valuable source of information in studies of global climate change and the evolution of present day life forms. Increasingly sea ice is being used as a proxy for extraterrestrial ice covered systems. Sea Ice provides a comprehensive review of our current available knowledge of polar pack ice, the study of which is severely constrained by the logistic difficulties of working in such harsh and remote regions of the earth. The book’s editors, Drs Thomas and Dieckmann have drawn together an impressive group of international contributing authors, providing a well-edited and integrated volume, which will stand for many years as the standard work on the subject. Contents of the book include details of the growth, microstructure and properties of sea ice, large-scale variations in thickness and characteristics, its primary production, micro-and macrobiology, sea ice as a habitat for birds and mammals, sea ice biogeochemistry, particulate flux, and the distribution and significance of palaeo sea ice. Sea Ice is an essential purchase for oceanographers and marine scientists, environmental scientists, biologists, geochemists and geologists. All those involved in the study of global climate change will find this book to contain a wealth of important information. All libraries in universities and research establishments where these subjects are studied and taught will need multiple copies on their shelves. David Thomas is at the School of Ocean Sciences, University of Wales, Bangor, UK. Gerhard Dieckmann is at the Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany
Download or read book The Drift of Sea Ice written by Matti Leppäranta and published by Springer Science & Business Media. This book was released on 2007-03-06 with total page 282 pages. Available in PDF, EPUB and Kindle. Book excerpt: This book presents the fundamental laws of sea ice drift, as derived from the material properties of sea ice, the basic laws of mechanics, and the latest modeling techniques. Topics covered include the science of sea ice drift, forecasting velocity based on volume, size and shape, sea ice ridging and remote sensing, modelling of ice conditions, and the role of sea ice drift in oceanography, marine ecology and engineering.
Download or read book Air Ice Ocean Interaction written by Miles McPhee and published by Springer. This book was released on 2008-09-10 with total page 0 pages. Available in PDF, EPUB and Kindle. Book excerpt: At a time when the polar regions are undergoing rapid and unprecedented change, understanding exchanges of momentum, heat and salt at the ice-ocean interface is critical for realistically predicting the future state of sea ice. By offering a measurement platform largely unaffected by surface waves, drifting sea ice provides a unique laboratory for studying aspects of geophysical boundary layer flows that are extremely difficult to measure elsewhere. This book draws on both extensive observations and theoretical principles to develop a concise description of the impact of stress, rotation, and buoyancy on the turbulence scales that control exchanges between the atmosphere and underlying ocean when sea ice is present. Several interesting and unique observational data sets are used to illustrate different aspects of ice-ocean interaction ranging from the impact of salt on melting in the Greenland Sea marginal ice zone, to how nonlinearities in the equation of state for seawater affect mixing in the Weddell Sea. The book’s content, developed from a series of lectures, may be appropriate additional material for upper-level undergraduates and first-year graduate students studying the geophysics of sea ice and planetary boundary layers.
Download or read book The Geophysics of Sea Ice written by Norbert Untersteiner and published by Springer. This book was released on 2013-12-19 with total page 1197 pages. Available in PDF, EPUB and Kindle. Book excerpt: Based on the proceedings of the NATO Advanced Study Institute on Air-Sea-Ice Interaction held September 28-October 10, 1981 in Acquafredda di maratea, Italy. Intent is to present the topic of sea ice in the broad and interdisciplinary context of atmospheric and oceanographic science.
Download or read book Air Ice Ocean Interaction written by Miles McPhee and published by Springer Science & Business Media. This book was released on 2008-06-04 with total page 218 pages. Available in PDF, EPUB and Kindle. Book excerpt: At a time when the polar regions are undergoing rapid and unprecedented change, understanding exchanges of momentum, heat and salt at the ice-ocean interface is critical for realistically predicting the future state of sea ice. By offering a measurement platform largely unaffected by surface waves, drifting sea ice provides a unique laboratory for studying aspects of geophysical boundary layer flows that are extremely difficult to measure elsewhere. This book draws on both extensive observations and theoretical principles to develop a concise description of the impact of stress, rotation, and buoyancy on the turbulence scales that control exchanges between the atmosphere and underlying ocean when sea ice is present. Several interesting and unique observational data sets are used to illustrate different aspects of ice-ocean interaction ranging from the impact of salt on melting in the Greenland Sea marginal ice zone, to how nonlinearities in the equation of state for seawater affect mixing in the Weddell Sea. The book’s content, developed from a series of lectures, may be appropriate additional material for upper-level undergraduates and first-year graduate students studying the geophysics of sea ice and planetary boundary layers.
Download or read book The Role of Ocean Heat Transport on Rapid Sea Ice Declines in the Community Earth System Model Large Ensemble written by Gabriel Auclair and published by . This book was released on 2018 with total page pages. Available in PDF, EPUB and Kindle. Book excerpt: "Many climate models predict future rapid sea ice declines in the Arctic. These events are linked with anomalous northward Ocean Heat Transport (OHT). Using the Community Earth System Model Large Ensemble (CESM-LE), we find that the partitioning of the poleward OHT between the different gates of the Arctic (Barents Sea Opening (BSO), Fram Strait or Bering Strait) is key to this link with the rapid declines. In total, 64 of the 79 rapid declines in CESM-LE are linked with anomalous OHT. The interaction between OHT and sea ice happens mainly over continental shelves. The Bering Strait OHT is linked to more rapid declines than the BSO OHT, presumably because of the broader Eurasian shelf. No clear link is found between rapid declines and the OHT through the Fram Strait, which is a deep gate to the Arctic Ocean, except when the rapid decline is also linked to the BSO or Bering Strait OHTs. When the September Sea Ice Extent (SIE) before the rapid decline is located only over deep basins in the central Arctic, we observe a decrease in basal melt during the decline. We hypothesize that this is due to an enhanced stratification that reduces heat transfer between the ocean and the ice. The ice-atmosphere heat flux anomalies are more strongly correlated with the sea ice concentration anomalies over the deep basins in the 21st century than the ice-ocean heat flux anomalies. Our results suggest that OHTs are causing rapid sea ice declines mostly when the SIE is large enough to cover the continental shelves and that the atmosphere is the main driver when the initial SIE is located only over the deep basins." --
Download or read book Ice Drift Ocean Circulation and Climate Change written by Jens Bischof and published by Springer Science & Business Media. This book was released on 2000-11 with total page 254 pages. Available in PDF, EPUB and Kindle. Book excerpt: The issue of global warming and climate change is of continuous concern. Since the 1970s, it bas been shown that the pack-ice around the Arctic Ocean is thinning, the margin of permafrost is moving north and the vegetation in the high northern parts of the world is changing (the 'greening' of the Arctic). But are these changes the result of human activity or simply regular variations of the Earth's climate system? Over thousands of years, a continuous archive of iceberg and sea ice drift bas formed in the deep-sea sediments, revealing the place of the ice's origin and allowing a reconstruction of the surface currents and the climate of the past. However, the drift of floating ice from one place to another is not just a passive record of past ocean circulation. It actively influences and changes the surface ocean circulation, thus having a profound effect on climate change. Ice Drift, Ocean Circulation and Climate Change is the first book to focus on the interactions between ice, the ocean and the atmosphere and to describe how these three components of the climate system influence each other. It makes clear the positive contribution of paleoclimatology and paleoceanography and should be read by anyone concerned with global warming and climate change.
Download or read book Ice Dynamics written by William D. Hibler and published by . This book was released on 1984 with total page 72 pages. Available in PDF, EPUB and Kindle. Book excerpt: This monograph reviews essential aspects of sea ice dynamics on the geophysical scale and discusses the role of ice dynamics in air-sea-ice interaction. The review is divided into the following components: (a) a discussion of the momentum balance describing ice drift, (b) an examination of the nature of sea ice rheology on the geophysical scale, (c) an analysis of the relationship between ice strength and ice thickness characteristics, and (d) a discussion of the rle of ice dynamices in the atmosphere-ice-ocean system. Because of the unique, highly nonlinear nature of sea-ice interaction, special attention is given to the ramifications of ice interaction on sea ice motion and deformation. These ramifications are illustrated both by analytic solution and by numerical model results. In addition, the role of ice dynamics in the atmosphere-ice-ocean system is discussed in light of numerical modeling experiments, including a fully coupled ice-ocean model of the Arctic-Greenland-Norwegian seas.
Download or read book The Role of Waves in the Autumn Arctic Ocean written by Madison Smith and published by . This book was released on 2019 with total page 161 pages. Available in PDF, EPUB and Kindle. Book excerpt: Recent decline of sea ice coverage in the Arctic Ocean has resulted in a substantial seasonal wave climate. Waves generated in the open water are attenuated far into the sea ice, but are a defining feature of the marginal ice zone (MIZ). In autumn, waves in the MIZ can be large due to the significant open water area following the minimum ice extent. Waves are expected to affect ice cover development through both kinematic and thermodynamic processes. In this research, I use observations from 2015 in the Beaufort Sea region to improve understanding of key feedbacks between waves and sea ice, and describe implications for autumn ice formation. In the MIZ, where surface waves are often present, much of the ice forms through the 'pancake cycle'. Gradients in wave orbital velocities across the surface cause small ice crystals to be herded into increasingly larger, rounded floes. Modeling the relative motion between ice floes is the basis for describing pancake ice growth, as well as the attenuation of wave energy associated with their motion. Here, existing models for ice motion and growth are evaluated using coincident measurements of waves and pancake sea ice made using shipboard stereo video. The observations are well captured by existing models, and relative velocities of floes are typically small compared to the mean orbital velocities. The models for relative motion of pancake sea ice due to waves can be subsequently used to estimate attenuation of wave energy due to floe motion. Under the conditions observed, estimates of wave energy loss from ice-ocean turbulence are much larger than those from pancake collisions, and can account for most of the observed wave attenuation. In addition to the general trends of sea ice growth in the Arctic in autumn, ice edge advance can be temporarily reversed as a result of upper ocean mixing by wind and waves. Observations during a high wind and wave event demonstrate how heat released from the upper ocean can melt significant amounts of newly formed pancake sea ice. Measurements from drifting buoys and ship-based platforms are used to construct heat and salt budgets, which give a consistent picture of the air-ice-ocean evolution. Following the event, there was less heat remaining in the upper ocean and sea ice formation quickly resumed. The young ice cover formed throughout the autumn significantly changes the way in which momentum is transferred from the wind to the waves, and into the ocean below. Using coincident measurements of sea ice, wind, surface waves, and near-surface turbulence across a range of conditions, I quantify the relationship between new sea ice formation, attenuation of waves, and suppression of near-surface turbulence. Sea ice formation reduces the wind input transfer velocity by attenuating the short waves, which simultaneously suppresses the wave-driven near-surface turbulence. As ice thickens and grows, the ice provides the dominant roughness for wind input. Based on the observations, I suggest parameters for estimating near-surface turbulence in thin pancake and frazil ice, which are ubiquitous in autumn marginal ice zones. The results of this research provide validation and parameterization for a new class of sea ice models that include dynamic and thermodynamic floe processes. Constraining rates of pancake ice growth is important as it occurs at a much faster rate than simple thermodynamic ice growth, and it is believed to be more common in the Arctic Ocean in recent years. Yet, as the timing of the ice-edge advance shifts later into stormier autumn months, waves from storm events may play an increasing role in delaying ice advance. Thus, the coupled wave-ice interactions examined are likely to become increasingly important in determining the state of the autumn Arctic Ocean with the growing wave climate.
Download or read book Proceedings of the Symposium on Ice Ocean Dynamics and Mechanics Held at Hanover New Hampshire USA 26 31 August 1990 written by and published by . This book was released on 1991 with total page 298 pages. Available in PDF, EPUB and Kindle. Book excerpt: Papers and abstracts from the Symposium on Ice-Ocean Dynamics, including sea-ice dynamics, sea-ice mechanics, ice-plate dynamics and mechanics, local ice-ocean interaction phenomena, relict flow stripes, and atmosphere-ice-ocean interactions in both the Arctic and Antarctic.
Download or read book Field Techniques for Sea Ice Research written by Hajo Eicken and published by University of Alaska Press. This book was released on 2010-03-15 with total page 590 pages. Available in PDF, EPUB and Kindle. Book excerpt: As much as one-tenth of the world’s oceans are covered with sea ice, or frozen ocean water, at some point during the annual cycle. Sea ice thus plays an important, often defining, role in the natural environment and the global climate system. This book is a global look at the changes in sea ice and the tools and techniques used to measure and record those changes. The first comprehensive research done on sea-ice field techniques, this volume will be indispensable for the study of northern sea ice and a must-have for scientists in the field of climate change research.
Download or read book On the Relation Between the Ice Transport in the East Greenland Current and the Atmospheric Circulation Over the Arctic Ocean written by Klaus Strübing and published by . This book was released on 1980 with total page 16 pages. Available in PDF, EPUB and Kindle. Book excerpt:
