中大機構典藏-NCU Institutional Repository-提供博碩士論文、考古題、期刊論文、研究計畫等下載:Item 987654321/27671
English  |  正體中文  |  简体中文  |  全文笔数/总笔数 : 78852/78852 (100%)
造访人次 : 36179130      在线人数 : 702
RC Version 7.0 © Powered By DSPACE, MIT. Enhanced by NTU Library IR team.
搜寻范围 查询小技巧:
  • 您可在西文检索词汇前后加上"双引号",以获取较精准的检索结果
  • 若欲以作者姓名搜寻,建议至进阶搜寻限定作者字段,可获得较完整数据
  • 进阶搜寻


    jsp.display-item.identifier=請使用永久網址來引用或連結此文件: http://ir.lib.ncu.edu.tw/handle/987654321/27671


    题名: A land surface process radiobrightness model with coupled heat and moisture transport in soil
    作者: Liou,YA;England,AW
    贡献者: 太空及遙測研究中心
    关键词: MICROWAVE DIELECTRIC BEHAVIOR;LOW-LEVEL PARAMETERS;WATER-CONTENT;SEQUENTIAL ASSIMILATION;HYDRAULIC CONDUCTIVITY;UNSATURATED SOILS;MASS-TRANSFER;WET SOIL;TEMPERATURE;EVAPORATION
    日期: 1998
    上传时间: 2010-06-29 18:51:52 (UTC+8)
    出版者: 中央大學
    摘要: Heat and moisture transport in soil are coupled processes that jointly determine temperature and moisture profiles, We present a physically based, one-dimensional (1-D), coupled heat and moisture transport hydrology (1-DH) model for bare, unfrozen, moist soils subject to insolation, radiant heating and cooling, and sensible and latent heat exchanges with the atmosphere. A 60-day simulation is conducted to study the effect of dry-down on soil temperature and moisture distributions in summer for bare soil in the Midwest United States, Given a typical initial moisture content of 38% by volume, we find that temperature differences between the water transport and no water transport cases exhibit a diurnal oscillation with a slowly increasing amplitude, but never exceed 4.4 K for the 60-day period, However, moisture content of the surface decreases significantly with time for the water transport case and becomes only about 21% at the end of the same period, The 1-DH model is linked to a radiobrightness (1-DH/R) model as a potential means for soil moisture inversion, The model shows that radiobrightness thermal inertia (RTI) correlates with soil moisture if the two radiobrightnesses are taken from times near the thermal extremes, e.g., 2 a.m. and 2 p.m., and that RTI appears temperature-dependent at the ending stages of the dry-down simulations where soils are dry and their moisture contents vary slowly, Near times of thermal crossover, the RTI technique is insensitive to soil moisture.
    關聯: IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING
    显示于类别:[太空及遙測研究中心] 期刊論文

    文件中的档案:

    档案 描述 大小格式浏览次数
    index.html0KbHTML679检视/开启


    在NCUIR中所有的数据项都受到原著作权保护.

    社群 sharing

    ::: Copyright National Central University. | 國立中央大學圖書館版權所有 | 收藏本站 | 設為首頁 | 最佳瀏覽畫面: 1024*768 | 建站日期:8-24-2009 :::
    DSpace Software Copyright © 2002-2004  MIT &  Hewlett-Packard  /   Enhanced by   NTU Library IR team Copyright ©   - 隱私權政策聲明