An electrothermody namic model with distributed properties for effective perrnittivities of sea ice
نویسندگان
چکیده
This paper presents a model to calculate tile tcInperature de-pmclcncc of effective permit tivit ies for a 1 Ietero?;eneous anisotropic medium containing multiphase scatterers. With the strong pcrmit-tivity fluctuation approach, the mc)del is developed to account for the clcctrodynamic scattering effect together with the cluasi-static characteristics of multiple spccics and sulxpecics of inhomogencities with distributed orientations, sizes, and sl)apcs. DUC to a preferential direction in the orientation distribution, the medium is effectively 2 anisotropic. The size distribution is described with a probability density function in terms of normalized volumetric sizes. Scatterer shapes arc ncmunifcmn and have a genera] ellipsoidal form cllaracterizcxl by arbitrary axial ratios of correlation lengths which arc related to physical geometries of the scatterers. In tl]is formulation, sca ice consisting c)f solid ice, liquicl brine, and gaseous inclusions is moclelcd to derive a.nisotropic cffcctivc pcmnittivitics with thcrmodyrlamic phase redistribution and structural l]letal~lor])llis]l],, Theoretical results arc in goocl agrmxncnt with experimental data at 4.8 GHz for saline ice undergoing warming and cooling cycles. A competitive effect between the increase of liquid brine and the rouxidi]lg of ellipsoidal scatterers at increasing temperatures explains the trend observed in measured data. Sensitivities of cffcctivc permittivities to structural ancl physical parameters characterizing sea ice arc also studied.
منابع مشابه
Polarimetric signatures of sea ice 1. Theoretical model
Physical, structural, and electromagnetic properties and interrelating processes in sea ice are used to develop a composite model for polarimetric backscattering signatures of sea ice. Physical properties of sea ice constituents such as ice, brine, air, and salt are presented in terms of their effects on electromagnetic wave interactions. Sea ice structure and geometry of scatterers are related...
متن کاملPolarimetric signatures of sea ice Part I: Theoretical model
Physical, structural, and electromagnetic properties and interrelating processes in sea ice are used to develop a composite model for po-larimetric backscattering signatures of sea ice. Physical properties of sea ice constituents such as ice, brine, air, and salt are presented in terms of their effects on electromagnetic wave interactions. Sea ice structure and geometry of scatterers are relate...
متن کاملM96-1 for web
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 t...
متن کاملA Combination of Feature Tracking and Pattern Matching with Optimal Parametrization for Sea Ice Drift Retrieval from SAR Data
Sea ice drift strongly influences sea ice thickness distribution and indirectly controls air-sea ice-ocean interactions. Estimating sea ice drift over a large range of spatial and temporal scales is therefore needed to characterize the properties of sea ice dynamics and to better understand the ongoing changes of the climate in the polar regions. An efficient algorithm is developed for processi...
متن کاملInfluence of stochastic sea ice parametrization on climate and the role of atmosphere-sea ice-ocean interaction.
The influence of a stochastic sea ice strength parametrization on the mean climate is investigated in a coupled atmosphere-sea ice-ocean model. The results are compared with an uncoupled simulation with a prescribed atmosphere. It is found that the stochastic sea ice parametrization causes an effective weakening of the sea ice. In the uncoupled model this leads to an Arctic sea ice volume incre...
متن کامل