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研究生:彭蘭馨
研究生(外文):Peng, Lan-Hsin
論文名稱:利用衛星影像求取山區部份地表反射率
論文名稱(外文):Estimation of Canopy Reflectance around Mountainous Area using Satellite Remotely Sensed Imagery
指導教授:王顯達王顯達引用關係
指導教授(外文):Wang Hsien-Ta
學位類別:碩士
校院名稱:國立中央大學
系所名稱:太空科學研究所
學門:自然科學學門
學類:天文及太空科學學類
論文種類:學術論文
論文出版年:1997
畢業學年度:85
語文別:中文
論文頁數:75
中文關鍵詞:山區反射率分類
外文關鍵詞:mountainreflectanceclassification
相關次數:
  • 被引用被引用:1
  • 點閱點閱:188
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  • 下載下載:0
  • 收藏至我的研究室書目清單書目收藏:0
摘要 如何能夠由山區衛星影像求取地表反射率,真實地反應出山區地表
的訊息,是在山區遙測應用上最重要的課題之一。本文的目的即在探討如
何利用山區TM影像,配合數值地形模型(DTM)資料及實測之大氣穿透率,
以估算出山區地表多方性反射率,提高山區地物分類之準確度,並且提供
大氣模式之制約條件,可用來修正大氣模式。 利用同種地物在太陽直射
區與陰影區輻射強度之差值,可得到地表反射太陽直射輻照度至感應器之
輻射強度,再配合數值地形模型,及實測之大氣穿透率值,就可求得山區
在太陽直射區之地表反射率。當某種地物在陰影區之像元數目太少時,其
陰影區之輻射強度可由該高程全部陰影區之平均輻射強度代替之。 山區
地物之反射率是三方向性的,是太陽入射方向、衛星觀測方向及地面法線
方向之函數。 首先,我們假設雙方向反射特性與地形(坡度坡向)變化
對山區地表反射率的影響是獨立的。而對於同一像元,各波段受到地形效
應的影響是一樣的。山區地物之雙方反射特性可由對平地地物雙方向反射
特性之研究中獲得。在本研究中,我們假設山區地物反射率之雙方向特性
與波段無關。因此,我們可藉由各波段反射率除以所有波段反射率之和,
求得各波段之相對百分比反射率,消除了地形效應及反射率之雙方向性效
應,而所得到的相對百分比反射率只和地物之本身的物理性質有關,因此
很適合做用來山區地物之分類。 本研究選取北台灣桃、竹、苗山區為試
區以計算出地表反射率。求取山區地表反射率所需之大氣穿透率是利用
Lowtran-7程式套計算得之,而Lowtran-7所需輸入的氣象程距值則由影像
上水體像元的灰度值估計得。本研究最後對山區地表之相對百分比反射率
影像做非監督式分類,共分得十一類,再由TM4的相對百分比反射率值判
斷,顯示其中十類為植被及一類為裸露地。

Estimation of Canopy Reflectance around Mountainous Areausing
Satellite Remotely Sensed Imagery.AbstractHow to estimate the
reflectance around mountainous area and interpretthe canopy
information with fidelity is one important task in the
remotelysensed application around mountainous area. The aim of
this paper is todiscuss that how to use Landsat TM, Digital
Terrain Model( DTM) and measuredatmospheric transmittance to
estimate the multi-directional reflectancearound mountainous
area. The final goal is to use these results to improvethe
classification accuracy of mountainous area, and provide the
constraintinformation for correcting atmospheric radiance/
transmittance computationmodels in the future.By computing the
radiant difference of same ground classes in the
directlyincident solar area and the shadow area, The reflected
solar irradianceobserved by satellite-borne sensors can be
gotten. With the aid of DTM andtransmittance data, we can
compute the reflectance around the directlyincident solar area.
In this computation, the radiance values around shadowarea could
be replaced with the average radiance of all shadow pixels in
thesame high range. The reflectance of mountainous canopy is
dependent on threedirection factors, incident solar direction,
satellite observed direction andsurface normal direction. In
this study, we assume the contributions of bi-directional
reflectance function and topographic effect( slope and
azimuthdirection) to reflectance are indepent, and the
topographic effect for thesame pixels in different bands are
same. The bi-directional reflectanceproperty can be gotten from
the analysis of the plain canopy area. So, wecan eliminate the
bi-directional effect and topographic by deriving thepercent
reflectance in each band. The percent reflectance is calculated
bydividing the reflectance by the sum of all bands' reflectance.
Owing to thepercent reflectance only dependent on the canopy
class' spectrum property,it is more proper to the classification
work than the original(absolute)reflectance. This study adopted
the Northern Taiwan mountainous area, including Taoyuan, Hsintzu
and Miauli mountainous area, as our test area. We used Lowtran7
model to compute the atmospheric transmittance, which the input
meteorological range for Lowtran7 was estimated from the
waterbody pixels' counts in TM images. Finally, this study used
unsupervise classification to classify the computed reflectance.
The result showed that 11 classes were classified. Justify by
the aid of the reflectance values in TM4 band, 10 classes in
them were vegetables and the other was soil canopies.

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