ADEOS-II/GLI snow/ice products - Part I: Scientific basis

被引:50
作者
Stamnes, Knut
Li, Wei [1 ]
Eide, Hans
Aoki, Teruo
Hori, Masahiro
Storvold, Rune
机构
[1] Stevens Inst Technol, Dept Phys & Engn Phys, Light & Life Lab, Hoboken, NJ 07030 USA
[2] Univ Oslo, N-0316 Oslo, Norway
[3] Meteorol Res Inst, Tsukuba, Ibaraki 3050052, Japan
[4] Earth Observ Res Ctr, Japan Aerosp Explorat Agcy, Tsukuba, Ibaraki 3058505, Japan
[5] NORUT Informat Technol Ltd, N-9294 Tromso, Norway
关键词
cloud masking; snow grain size; snow impurity;
D O I
10.1016/j.rse.2007.03.023
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Algorithms for retrieval of aerosol and snow/ice properties in polar and mid-latitude regions are described. These include (i) a cloud mask, (ii) a snow/sea ice discriminator, (iii) algorithms for retrieval of snow properties (snow grain size and impurities) and (iv) surface temperature of snow/ ice and open ocean water. The cloud mask and snow/ice discriminator are used for cloud clearing as well as surface classification. For cloud-free pixels that are determined to be snow-covered an algorithm for retrieval of snow grain size and impurity concentration has been constructed. Radiative transfer simulations of the coupled atmosphere-surface system are used to construct lookup tables that are used in the retrieval process which proceeds by comparing measured top-of-the-atmosphere (TOA) radiances with synthetic values obtained from the lookup tables. These algorithms are designed to be applicable to polar and mid-latitude regions, but can easily be extended for use in other regions with seasonal and permanent snow-cover. The surface temperature retrieval algorithm consists of two parts: one for retrieval of the snow/ice surface temperature (IST), and another one for the retrieval of open-ocean surface temperature (SST). A multilinear regression technique is used to determine the empirical coefficients in the expression for the surface temperature, and Arctic radiosonde data are used in conjunction with radiative transfer models to simulate the sensor-measured radiances. The algorithms have been extensively tested against synthetic data, Moderate Resolution Imaging Spectroradiometer (MODIS), MODIS Airborne Simulator (MAS) and GLobal Imager (GLI) data as well as other data sources. (c) 2007 Elsevier Inc. All rights reserved.
引用
收藏
页码:258 / 273
页数:16
相关论文
共 81 条
  • [1] Ackerman S, 1997, Discriminating Clear-Sky From Cloud With MODIS Algorithm Theoretical Basis Document (MOD35)
  • [2] [Anonymous], AERONAUTICS AEROSPAC
  • [3] [Anonymous], RADIATIVE TRANSFER A
  • [4] Numerical simulation of the atmospheric effects on snow albedo with a multiple scattering radiative transfer model for the atmosphere-snow system
    Aoki, T
    Aoki, T
    Fukabori, M
    Uchiyama, A
    [J]. JOURNAL OF THE METEOROLOGICAL SOCIETY OF JAPAN, 1999, 77 (02) : 595 - 614
  • [5] Effects of snow physical parameters on spectral albedo and bidirectional reflectance of snow surface
    Aoki, T
    Aoki, T
    Fukabori, M
    Hachikubo, A
    Tachibana, Y
    Nishio, F
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2000, 105 (D8) : 10219 - 10236
  • [6] AOKI T, 2007, REMOTE SENS ENVIRON, V111, P320
  • [7] Aoki T., 1998, POLAR METEOROL GLACI, V12, P1
  • [8] ADEOS-II/GLI snow/ice products - Part II: Validation results using GLI and MODIS data
    Aoki, Teruo
    Hori, Masahiro
    Motoyoshi, Hiroki
    Tanikawa, Tomonori
    Hachikubo, Akihiro
    Sugiura, Konosuke
    Yasunari, Teppel J.
    Storvold, Rune
    Eide, Hans A.
    Stamnes, Knut
    Li, Wei
    Nieke, Jens
    Nakajima, Yukinori
    Takahashi, Fumihiro
    [J]. REMOTE SENSING OF ENVIRONMENT, 2007, 111 (2-3) : 274 - 290
  • [9] BARTON IJ, 1985, J CLIM APPL METEOROL, V24, P508, DOI 10.1175/1520-0450(1985)024<0508:TMAGTI>2.0.CO
  • [10] 2