Research on the distribution and content of water ice in lunar pole regions using Clementine UVVIS data
Research on the distribution and content of water ice in lunar pole regions using Clementine UVVIS data
复制标题
利用Clementine UVVIS数据研究月极地区水冰分布和含量
DOI:
10.1007/s12583-011-0210-9
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发表时间:
2011-09
影响因子:
3.3
通讯作者:
Zhou, Chao
中科院分区:
文献类型:
--
作者:
Meng, Zhiguo;Chen, Shengbo;Lu, Peng;Wang, Zijun;Lian, Yi;Zhou, Chao
Interest in the Moon started to increase at the beginning of the 21st century, and henceforth, more and more attention has been paid to the content and distribution of water ice in the lunar polar regions. The existence of water or ice in the regolith can apparently change its dielectric features. Therefore, in this article, the Dobson model is adopted and improved according to the Moon’s environmental features, to construct the relationship between the volumetric water ice content and the dielectric constant. Thereafter, a lunar regolith dielectric distribution map is generated based on the improved Dobson model and the Clementine UVVIS data. The map indicates that the imaginary part of the dielectric constants in the lunar mare is much higher than that in the highlands. However, the maximum dielectric constants occur at the north- and south-pole regions, whose values are apparently bigger than those in the middle and low latitudes. Then, an abnormal map of the dielectric constant is gained if the threshold is put as 0.053 7, which is the highest value in the middle and low latitudes. The statistical results indicate that the number of abnormal pixels is 110 596, and the average is about 0.057 9. Assuming that the mean dielectric constant in the lunar mare is the normal dielectric constant at the south and north poles andɛ1=11.58+i0.057 9 is the abnormal one, the volumetric water ice content can be evaluated using the advanced Dobson model. The results show that the average volumetric water ice content is about 1.64%, and the total area is about 25 294 km2, where 10 956 km2belongs to the north pole and the rest is in the south pole.
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影响因子:
--
作者:
R. Hodges
通讯作者:
R. Hodges
影响因子:
--
作者:
B. Butler
通讯作者:
B. Butler
DOI:
10.1109/tgrs.1985.289498
发表时间:
1985-01-01
影响因子:
8.2
作者:
DOBSON, MC;ULABY, FT;ELRAYES, MA
通讯作者:
ELRAYES, MA
影响因子:
--
作者:
S. Nozette;P. Spudis;M. Robinson;D. B. J. Bussey;C. Lichtenberg;R. Bonner
通讯作者:
S. Nozette;P. Spudis;M. Robinson;D. B. J. Bussey;C. Lichtenberg;R. Bonner
DOI:
10.1007/s11430-009-0201-1
发表时间:
2010-03
期刊:
Science China Earth Sciences
影响因子:
--
作者:
WeiGuo Zhang;Jingshan Jiang;Heguang Liu;Xiaohui Zhang;Dehai Zhang;Dihui Li;ChuanDong Xu
通讯作者:
WeiGuo Zhang;Jingshan Jiang;Heguang Liu;Xiaohui Zhang;Dehai Zhang;Dihui Li;ChuanDong Xu