The Optical Properties of Young Sea Ice PDF Download
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Author: Donald Kole Perovich
Publisher:
ISBN:
Category : Ice
Languages : en
Pages : 151
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Book Description
Laboratory experiments.
Author: Donald Kole Perovich
Publisher:
ISBN:
Category : Ice
Languages : en
Pages : 151
Get Book Here
Book Description
Laboratory experiments.
Author: Donald K. Perovich
Publisher:
ISBN:
Category : Albedo
Languages : en
Pages : 34
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Book Description
Sea ice is a translucent material with an intricate structure and complex optical properties. Understanding the reflection, absorption, and transmission of shortwave radiation by sea ice is important to a diverse array of scientific problems, including those in ice thermodynamics and polar climatology. Radiative transfer in sea ice is a combination of absorption and scattering. Differences in the magnitude of sea ice optical properties are due primarily to differences in scattering. Spectral variations are mainly a result of absorption. Changes in such optical properties as the albedo, reflectance, transmittance, and extinction coefficient are directly related to changes in the state and structure of the ice. Physical changes that enhance scattering, such as the formation of air bubbles due to brine drainage, result in larger albedos and extinction coefficients. The albedo is quite sensitive to the surface state. If the ice has a snow cover, albedos are large. In contrast, the presence of liquid water on a bare ice surface causes a decrease in albedo, which is more pronounced at longer wavelengths. Sea-ice optical properties depend on the volume of brine and air and on how the brine and air are distributed.
Author: David D. Erickson
Publisher:
ISBN:
Category : Sea ice
Languages : en
Pages : 158
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Book Description
Author: Holly J. Reay
Publisher:
ISBN:
Category :
Languages : en
Pages :
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Book Description
Author: David N. Thomas
Publisher: John Wiley & Sons
ISBN: 1118778383
Category : Science
Languages : en
Pages : 666
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Book Description
Over the past 20 years the study of the frozen Arctic and Southern Oceans and sub-arctic seas has progressed at a remarkable pace. This third edition of Sea Ice gives insight into the very latest understanding of the how sea ice is formed, how we measure (and model) its extent, the biology that lives within and associated with sea ice and the effect of climate change on its distribution. How sea ice influences the oceanography of underlying waters and the influences that sea ice has on humans living in Arctic regions are also discussed. Featuring twelve new chapters, this edition follows two previous editions (2001 and 2010), and the need for this latest update exhibits just how rapidly the science of sea ice is developing. The 27 chapters are written by a team of more than 50 of the worlds’ leading experts in their fields. These combine to make the book the most comprehensive introduction to the physics, chemistry, biology and geology of sea ice that there is. This third edition of Sea Ice will be a key resource for all policy makers, researchers and students who work with the frozen oceans and seas.
Author: Donald K. Perovich
Publisher:
ISBN:
Category : Albedo
Languages : en
Pages : 19
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Book Description
The albedo and transmittance of melting, first‐year Arctic sea ice were measured during two cruises of the Impacts of Climate on the Eco‐Systems and Chemistry of the Arctic Pacific Environment (ICESCAPE) project during the summers of 2010 and 2011. Spectral measurements were made for both bare and ponded ice types at a total of 19 ice stations in the Chukchi and Beaufort Seas. These data, along with irradiance profiles taken within boreholes, laboratory measurements of the optical properties of core samples, ice physical property observations, and radiative transfer model simulations are employed to describe representative optical properties for melting first‐year Arctic sea ice. Ponded ice was found to transmit roughly 4.4 times more total energy into the ocean, relative to nearby bare ice. The ubiquitous surface‐scattering layer and drained layer present on bare, melting sea ice are responsible for its relatively high albedo and relatively low transmittance. Light transmittance through ponded ice depends on the physical thickness of the ice and the magnitude of the scattering coefficient in the ice interior. Bare ice reflects nearly three‐quarters of the incident sunlight, enhancing its resiliency to absorption by solar insolation. In contrast, ponded ice absorbs or transmits to the ocean more than three‐quarters of the incident sunlight. Characterization of the heat balance of a summertime ice cover is largely dictated by its pond coverage, and light transmittance through ponded ice shows strong contrast between first‐year and multiyear Arctic ice covers.
Author: Per Gloersen
Publisher:
ISBN:
Category : Glaciology
Languages : en
Pages : 24
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Book Description
Author:
Publisher:
ISBN:
Category : Cold regions
Languages : en
Pages : 306
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Book Description
Author:
Publisher:
ISBN:
Category :
Languages : en
Pages : 54
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Book Description
Time series studies of the spectral irradiance fields beneath multiyear pack ice were conducted in the Eastern Arctic Basin at 82-83 deg N as part of the Coordinated Eastern Arctic Research Experiment (CEAREX). Particulate matter was collected from the multiyear pack ice as well as first year ice in a refrozen lead. The vertical distribution within the ice and the spectral absorbtion properties of the particulates were determined in order to estimate their contribution to the optical properties of the sea ice. Among the particulates contained in sea ice detritus was common throughout all portions of the pack ice and was the major light absorbing particulate matter in the ice at the time of the observation. Algal cells and mineral-like particulates also were present, yet they contributed to the light-absorbing properties to a lesser extent than the detritus. During early spring, particulate matter contributed little to the bulk attenuation coefficients of the multiyear ice, however, it was estimated to have a more substantial contribution to the attenuation coefficients of first year ice in a refrozen lead. Results of a single stream multilayer radiative transfer model that simulates concentrations of biogenic particulate matter observed in Arctic sea ice indicates that particulate matter within sea ice plays a substantial role in radiative energy transfer and has the potential to seasonally alter spectral irradiance regimes within the ice covered Arctic ocean.
Author: Mohammed Shokr
Publisher: John Wiley & Sons
ISBN: 1119828163
Category : Science
Languages : en
Pages : 628
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Book Description
SEA ICE The latest edition of the gold standard in sea ice references In the newly revised second edition of Sea Ice: Physics and Remote Sensing, a team of distinguished researchers delivers an in-depth review of the features and structural properties of ice, as well as the latest advances in geophysical sensors, ice parameter retrieval techniques, and remote sensing data. The book has been updated to reflect the latest scientific developments in macro- and micro-scale sea ice research. For this edition, the authors have included high-quality photographs of thin sections from cores of various ice types, as well as a comprehensive account of all major field expeditions that have systematically surveyed sea ice and its properties. Readers will also find: A thorough introduction to ice physics and physical processes, including ice morphology and age-based structural features Practical discussions of radiometric and radar-scattering observations from sea ice, including radar backscatter and microwave emission The latest techniques for the retrieval of sea ice parameters from space-borne and airborne sensor data New chapters on sea ice thermal microwave emissions and on the impact of climate change on polar sea ice Perfect for academic researchers working on sea ice, the cryosphere, and climatology, Sea Ice: Physics and Remote Sensing will also benefit meteorologists, marine operators, and high-latitude construction engineers.
