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基于SRTM的地形因子提取方法研究
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國家自然科學(xué)基金項(xiàng)目(41771315、41501294)和國家重點(diǎn)研發(fā)計(jì)劃項(xiàng)目(2020YFD1100601)


Topographic Factor Extraction Method Based on SRTM
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    摘要:

    地形是影響土壤侵蝕的重要因子,,在侵蝕估算模型中常用坡度和坡長(zhǎng)(LS)來衡量,,在大區(qū)域上常基于數(shù)字高程模型(DEM)提取,。SRTM作為大區(qū)域尺度上質(zhì)量高,、易獲取的高程數(shù)據(jù),在全球土壤侵蝕評(píng)價(jià)中得到廣泛應(yīng)用,。但現(xiàn)有地形因子提取算法要求高程和柵格單元的單位(通常為m)一致,,需對(duì)SRTM進(jìn)行坐標(biāo)變換才能使用。針對(duì)大區(qū)域上SRTM坐標(biāo)轉(zhuǎn)換時(shí)間開銷大的問題,,提出了一種直接基于SRTM提取地形因子的算法(LSA-SRTM),。該算法利用地理坐標(biāo)系下的經(jīng)緯度信息計(jì)算柵格單元長(zhǎng)度及單元坡長(zhǎng),結(jié)合最陡坡降策略獲得坡度及流向,,進(jìn)而提取匯水面積,,根據(jù)坡度設(shè)置坡度截?cái)帱c(diǎn),根據(jù)匯水面積閾值設(shè)置溝道截?cái)帱c(diǎn),,經(jīng)正,、反遍歷后獲得累積坡長(zhǎng),采用CSLE的分段公式計(jì)算LS因子,。以Himmelblau-Orlandini數(shù)學(xué)曲面,、5個(gè)典型樣區(qū)的1″SRTM作為數(shù)據(jù)源,將LSA-SRTM,、投影坐標(biāo)系下的LS算法(LSA-DEM)與手工測(cè)量的結(jié)果進(jìn)行對(duì)比,。LSA-SRTM方法與測(cè)量值在數(shù)學(xué)曲面和典型樣區(qū),坡長(zhǎng)的R2分別為0.8552,、0.7788,、0.7269、0.7024,、0.6909,、0.7255,LS因子的R2分別為0.8907,、0.8209,、0.8213,、0.7142、0.7145,、0.8212,。在運(yùn)行時(shí)間方面,LSA-SRTM方法具有較高的效率,。結(jié)果表明,,LSA-SRTM算法計(jì)算精度、效率更高,,可為大區(qū)域地形因子提取的研究提供支撐,。

    Abstract:

    Topography is an important factor that affects soil erosion, which is usually measured by slope gradient and slope length (LS) in erosion estimation models, and extracted based on digital elevation model (DEM) on a vast area. SRTM, as currently high-quality and easily accessible elevation data on a vast area, has been applied in global soil erosion evaluation. However, the traditional algorithm for topographic factor extraction requires that the unit of elevation identical with cell size (usually meters), which makes SRTM need perform coordinate transformation before extraction. Aiming at the problem of high cost in performing coordinate transformation on SRTM data in a large area, an algorithm for extracting terrain factors directly was proposed based on SRTM (LSA-SRTM). The longitude and latitude information of the geographic coordinate system was used to directly calculate the cell size and the unit slope length. D8 method was used to acquire slope gradient and flow direction matrix. Then, the slope gradient cutoff was calculated according to the slope gradient result, the catchment area was calculated and the channel network cutoff was set, furtherly, the cumulative slope length was obtained by “forward-reverse traversal”. Finally, the LS factor was calculated according to the slope gradient, cumulative slope length and the segmentation formula of CSLE. Using Himmelblau-Orlandini mathematical surface and 1″SRTM of five typical samples in China as the data source, the LSA-SRTM method, the projected coordinate system DEM-based LS extraction algorithm (LSA-DEM) and manual measurement method were compared. On the mathematical surface and the typical sample area, the R2 of the slope length of LSA-SRTM method and the measured value were 0.8552, 0.7788, 0.7269, 0.7024, 0.6909 and 0.7255. The R2 of the LS and the measured value were 0.8907, 0.8209, 0.8213, 0.7142, 0.7145 and 0.8212. In terms of execution time, the LSA-SRTM method had high efficiency. The experiment results showed that the LSA-SRTM had higher accuracy and efficiency, which can provide a support for the study of topographic factor extraction in vast areas.

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張宏鳴,常毅,楊勤科,張泉,董良,許伊昆.基于SRTM的地形因子提取方法研究[J].農(nóng)業(yè)機(jī)械學(xué)報(bào),2022,53(1):205-214. ZHANG Hongming, CHANG Yi, YANG Qinke, ZHANG Quan, DONG Liang, XU Yikun. Topographic Factor Extraction Method Based on SRTM[J]. Transactions of the Chinese Society for Agricultural Machinery,2022,53(1):205-214.

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  • 收稿日期:2020-12-03
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  • 在線發(fā)布日期: 2022-01-10
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