Remote Sensing Technology and Application 鈥衡�� 2020, Vol. 35 鈥衡�� Issue (1): 120-131.DOI: 10.11873/j.issn.1004-0323.2020.1.0120

Previous Articles     Next Articles

Remotely Sensed Retrieving the Surface Soil Moisture of Yan鈥檃n Urban Forest based on Landsat Image and Trapezoid Method

Xinping Zhang1,2(),Zhi Qiao2,Hao Li2,Jie Yan2,Fangfang Zhang3,Dongfeng Zhao1,5,Dexiang Wang1(),Haibin Kang1,Hang Yang1,Yang Feng4   

  1. 1. College of Forestry, Northwest A&F University, Yangling 712100, China
    2. College of Art and Design, Xi鈥檃n University of Technology, Xi鈥檃n 710054, China
    3. Branch School of Gaoling District Xi鈥檃n City, Shaanxi Agricultural Broadcasting and Television School, Xi鈥檃n 710200, China
    4. College of Landscape Architecture and Arts, Northwest A&F University, Yangling 712100, China
    5. Yan'an Forestry Survey Planning and Design Institute, Yan'an 716000, China
  • Received:2018-08-16 Revised:2020-02-20 Online:2020-04-01 Published:2020-02-20
  • Contact: Dexiang Wang

鍩轰簬Landsat褰卞儚鍜屼笉瑙勫垯姊舰鏂规硶閬ユ劅鍙嶆紨寤跺畨鍩庡競妫灄琛ㄥ眰鍦熷¥姘村垎

寮犳柊骞�1,2(),涔旀不2,鏉庣殦2,闂澃2,寮犺姵鑺�3,璧垫爧閿�1,5,鐜嬪緱绁�1(),搴锋捣鏂�1,鏉ㄨ埅1,鍐壃4   

  1. 1. 瑗垮寳鍐滄灄绉戞妧澶у鏋楀闄紝闄曡タ 鏉ㄥ噷 712100
    2. 瑗垮畨鐞嗗伐澶у鑹烘湳涓庤璁″闄紝闄曡タ 瑗垮畨 710054
    3. 闄曡タ鐪佸啘涓氬箍鎾數瑙嗗鏍� 瑗垮畨甯傞珮闄靛垎鏍�, 闄曡タ 瑗垮畨 710200
    4. 瑗垮寳鍐滄灄绉戞妧澶у;椋庢櫙鍥灄涓庤壓鏈闄紝闄曡タ 鏉ㄥ噷 712100
    5. 寤跺畨甯傛灄涓氬嫎瀵熻鍒掕璁¢櫌锛岄檿瑗� 瑗垮畨 716000
  • 閫氳浣滆��: 鐜嬪緱绁�
  • 浣滆�呯畝浠�:寮犳柊骞筹紙1981-锛夛紝鐢凤紝闄曡タ鏌炴按浜猴紝璁插笀锛屽崥澹紝涓昏浠庝簨鏅瑙勫垝涓庨仴鎰熺洃娴嬬爺绌躲�侲?mail锛�jhonxinping81@nwsuaf.edu.cn銆�
  • 鍩洪噾璧勫姪:
    鍥藉鈥滃崄浜屼簲鈥濈鎶�鏀拺璁″垝璇鹃 鈥滅幆澧冨弸濂藉瀷鍩庨晣鏅鏋楁瀯寤烘妧鏈爺绌朵笌绀鸿寖鈥�(2015BAD07B06);鍥藉鑷劧绉戝鍩洪噾椤圭洰鈥滅Е宀澗鏍庢灄寤虹兢绉嶆洿鏂版牸灞�瀵圭瀛愭墿鏁h繃绋嬪強褰卞搷鍥犵礌鐨勫搷搴斺��(31470644);鏂囧寲閮ㄦ枃鍖栬壓鏈爺绌堕」鐩�滆タ鍖楀湴鍖哄伐涓氶仐浜у瀷浜т笟鍥湴鍩熸枃鍖栧垱鎰忓洜瀛愭鍏ュ強鏅娲诲寲鐮旂┒鈥�(17DH17);鏁欒偛閮ㄤ汉鏂囩ぞ绉戦潚骞村熀閲戦」鐩�滃伐涓氶仐浜у瀷鍒涙剰浜т笟鍥枃鍖栦紶鎵垮強鍦板煙璁ゅ悓鐮旂┒锛氬唴娑甸噸濉戙�佷笟鎬佸煿鑲层�佷富棰樿惀閫犫��(18YJC760063);闄曡タ鐪佺ぞ绉戠晫閲嶅ぇ鐞嗚涓庣幇瀹為棶棰樼爺绌堕」鐩�滃熀浜庣敓鎬佽瑙掔殑闄曡タ鍏充腑鍦板尯鍐滄潙浜哄眳鐜寤鸿妯″紡鐮旂┒鈥�(20192097)

Abstract:

It is crucial for soil moisture assessment to know the prediction accuracy of inversion model. Urban forest surface soil in a gully-loess region (Yan鈥檃n), was taken as the research object, and the three scenes of Landsat satellite remotely sensed imagery in different periods and soil moisture sensor in situ measurement data were used as the data source. The parameters of TOTRAM (Thermal-Optical TRApezoid Model) and OPTRAM (OPtical TRApezoid Model) were obtained through the scatter diagram of pixels in two-dimensional spaces (LST-NDVI and STR-NDVI, LSTis land surface temperature,NDVIis normalized vegetation index, and STR is shortwave infrared conversion reflection coefficient) and their fitting dry edge and wet edge, respectively. Then, the w values (soil moisture in percentage) of Yan鈥檃n urban forest were retrieved at the pixel level (30 m by 30 m), the accuracy of the two models was verified, the differences between the estimated results of the two models, and the influence of linear and nonlinear edge on the inversion results were compared. The results indicate that: (1) Except that the dry edge and wet edge of OPTRAM models on Landsat 7 and Landsat 8 were non-linear, the other dry and wet edges of pixels in LST-NDVI space and STR-NDVI space are almost linear and enveloped into a trapezoid shape. (2) Compared with the field measurement data, the mean error (ME) of TOTRAM and OPTRAM were 0.009 and 0.045 5, respectively, which indicating that the estimation results of both models were relatively high, but the root mean square error (RMSE) of the OPTRAM model was closer to zero than the TOTRAM model. The value of w estimated by the OPTRAM model is evenly distributed on both sides of the 1鈭�1 reference line, and the number of points on the reference line is more than that of the TOTRAM model in scatterplots, indicating that the accuracy of OPTRAM is higher than that of the TOTRAM model, moreover, the inversion precision of nonlinear edge is higher than that of linear edge. Thus, in further research, the relationship between the complexity of the dry edge and wet edge and the model鈥檚 accuracy improvement should be discussed in the OPTRAM model, and the influences of surrounding environment, rainfall, forest disturbance and NDVI saturation on the estimation accuracy of the two models need to be considered.

Key words: Normalized Difference Vegetation Index (NDVI), Soil moisture, Satellite remote sensing, Land surface temperature, Surface reflectance

鎽樿锛�

鍙嶆紨妯″瀷瀵瑰湡澹ゆ按鍒嗚瘎浼扮粨鏋滄湁閲嶈褰卞搷锛屽熀浜庢锛屼互榛勫湡娌熷鍖哄煄甯傛.鏋楄〃灞傚湡澹や负鐮旂┒瀵硅薄锛屼互3鏈烲andsat褰卞儚鍜屽疄鍦板湡澹ゆ按鍒嗕紶鎰熷櫒娴嬪畾鏁版嵁涓烘暟鎹簮锛屽垎鍒�氳繃鍍忓厓鍦ㄤ簩缁寸┖闂达紙LST-NDVI涓嶴TR-NDVI锛孡ST涓哄湴琛ㄦ俯搴︼紝NDVI涓哄綊涓�鍖栨琚寚鏁帮紝STR涓虹煭娉㈢孩澶栬浆鎹㈠弽灏勭郴鏁帮級涓殑鏁g偣鍥惧強鍏舵嫙鍚堢殑骞茬嚗杈圭晫涓庢箍娑﹁竟鐣岋紝鑾峰彇TOTRAM锛堢儹瀛︹�斿厜瀛︿笉瑙勫垯姊舰妯″瀷锛夊拰OPTRAM锛堝厜瀛︿笉瑙勫垯姊舰妯″瀷锛夌殑鍙傛暟锛岀劧鍚庡湪鍍忕礌姘村钩涓婏紙30 m脳30 m锛夊弽婕斿嚭寤跺畨鍩庡競妫灄琛ㄥ眰鍦熷¥姘村垎锛圵锛夛紝楠岃瘉涓ゆā鍨嬬殑绮惧害锛屽苟姣旇緝涓ゆā鍨嬩及绠楃粨鏋滅殑宸紓鍙婄嚎鎬ц竟鐣屼笌闈炵嚎鎬ц竟鐣屽鍙嶆紨缁撴灉鐨勫奖鍝嶃�傜粨鏋滃彂鐜帮細鈶犻櫎OPTRAM 妯″瀷鍦↙andsat 7鍜孡andsat 8涓婂共婀胯竟鐣屽憟鐜伴潪绾挎�у锛屽儚绱犲湪LST-NDVI绌洪棿鍜孲TR鈥擭DVI绌洪棿涓殑骞叉箍杈圭晫鍧囧憟绾挎�э紝涓斿寘缁滄垚涓嶈鍒欐褰㈠舰鐘�;鈶′笌瀹炲湴娴嬪畾鏁版嵁鐩告瘮锛孴OTRAM涓嶰PTRAM涓ゆā鍨嬬殑骞冲潎璇樊锛圡E锛夊垎鍒负0.009鍜�0.0455锛岃〃鏄庝袱妯″瀷浼扮畻缁撴灉鍧囧亸楂橈紝浣哋PTRAM妯″瀷鐨勫潎鏂规牴璇樊锛圧MSE锛夎緝TOTRAM妯″瀷鏇存帴杩�0銆侽PTRAM妯″瀷浼扮畻鐨刉鍊煎潎鍖�鍦板垎甯冨湪1鈭�1鍙傝�冪嚎涓や晶锛屼笖浣嶄簬鍙傝�冪嚎涓婄殑鐐规暟澶氫簬TOTRAM妯″瀷锛岃〃鏄嶰PTRAM鍑嗙‘搴﹂珮浜嶵OTRAM妯″瀷锛屼笖闈炵嚎鎬ц竟鐣岀殑鍙嶆紨绮惧害楂樹簬绾挎�ц竟鐣�;鈶笌TOTRAM妯″瀷鐩告瘮锛孫PTRAM妯″瀷浼扮畻鍑虹殑W绌洪棿鍒嗗紓瑙勫緥涓庡湡鍦板埄鐢�/瑕嗚绫诲瀷鍏锋湁杈冮珮鐨勭浉鍏虫�э紝涓擮PTRAM妯″瀷瀵规琚鐩栧害鏋佷綆鐨勫尯鍩熸晱鎰熴�傚洜姝わ紝鍦ㄥ悗缁爺绌朵腑锛屽簲鍦∣PTRAM妯″瀷涓帰璁ㄥ共婀胯竟鐣屽鏉傛�т笌妯″瀷鍑嗙‘鎬ф敼鍠勪箣闂寸殑鍏崇郴锛屽悓鏃惰�冭檻鍛ㄥ洿鐜銆侀檷闆ㄩ噺銆佹.鏋楀共鎵板拰NDVI楗卞拰绛夊洜绱犲涓ゆā鍨嬩及绠楀噯纭�х殑褰卞搷銆�

鍏抽敭璇�: 褰掍竴鍖栨琚寚鏁�, 鍦熷¥婀垮害, 鍗槦閬ユ劅, 鍦拌〃娓╁害, 鍦拌〃鍙嶅皠鐜�

CLC Number: