The behaviour of a surface temperature/vegetation index (TVX) matrix derived from 10‐day composite AVHRR images over monsoon Asia

Satellite remote sensing of surface-related variables is essential for understanding regional or global land-surface processes. This study focuses on a Temperature/Vegetation Index (TVX) matrix that combines surface temperature (Ts) and a normalized difference vegetation index (NDVI). The results of our study show the behaviour of the TVX matrix on continental scales. The study domain includes eastern Eurasia and monsoon Asia-regions with great variability in land-surface conditions. The data used included a 10-day composite Advanced Very High Resolution Radiometer (AVHRR) dataset compiled by the US Geological Survey (USGS). The relaxation in the determination algorithm for TVX slope (an upper envelope line in a TVX matrix box) was conducted to obtain both the negative and positive slope. The TVX slope can be derived from previous studies as the monsoon advanced and retreated over the tropics. However, over the Tibetan Plateau, a time series of the TVX slope showed an opposite sign compared to those in previous studies (represented by a positive TVX slope). Scatter plotting of the TVX matrix pixel sets was conducted for the evaluation of a variety of TVX matrix pixels. The TVX slope error sometimes occurred over arid regions because of a few green pixels corresponding to oases or irrigated areas. On the Tibetan Plateau, ‘two’ TVX slopes, both negative and positive, were found in the scatterplot. The reason for the two TVX slopes is the energy consumption in the soil, particularly, the phase change from frozen to liquid water. However, further study will be required to understand the mechanisms on the Plateau. Copyright © 2007 John Wiley & Sons, Ltd.

[1]  Richard K. Moore,et al.  Microwave remote sensing fundamentals and radiometry , 1981 .

[2]  S. Running,et al.  Estimation of regional surface resistance to evapotranspiration from NDVI and thermal-IR AVHRR data , 1989 .

[3]  Yann Kerr,et al.  Accurate land surface temperature retrieval from AVHRR data with use of an improved split window algorithm , 1992 .

[4]  Pedro Viterbo,et al.  The land surface‐atmosphere interaction: A review based on observational and global modeling perspectives , 1996 .

[5]  Tetsuzo Yasunari,et al.  The Seasonal and Intraseasonal Variability of Diurnal Cloud Activity over the Tibetan Plateau , 2001 .

[6]  C. Tucker,et al.  Climate-Driven Increases in Global Terrestrial Net Primary Production from 1982 to 1999 , 2003, Science.

[7]  J. Kondo,et al.  A Proper Method for Estimating Sensible Heat Flux above a Horizontal-Homogeneous Vegetation Canopy Using Radiometric Surface Observations , 1997 .

[8]  Bhaskar J. Choudhury,et al.  Analysis of normalized difference and surface temperature observations over southeastern Australia , 1991 .

[9]  B. Choudhury Multispectral satellite data in the context of land surface heat balance , 1991 .

[10]  T. Ohta,et al.  Seasonal variation in the energy and water exchanges above and below a larch forest in eastern Siberia , 2001 .

[11]  T. Carlson,et al.  Thermal remote sensing of surface soil water content with partial vegetation cover for incorporation into climate models , 1995 .

[12]  J. C. Price,et al.  Land surface temperature measurements from the split window channels of the NOAA 7 Advanced Very High Resolution Radiometer , 1984 .

[13]  Walter H. F. Smith,et al.  Free software helps map and display data , 1991 .

[14]  Kenji Tanaka,et al.  Surface Energy Budget at Amdo on the Tibetan Plateau using GAME/Tibet IOP98 Data. , 2001 .

[15]  J. Matsumoto Seasonal transition of summer rainy season over indochina and adjacent monsoon region , 1997 .

[16]  Takeshi Sato Spatial and Temporal Variations of Frozen Ground and Snow Cover in the Eastern Part of the Tibetan Plateau , 2001 .

[17]  E. Boegh,et al.  A Remote Sensing Study of the NDVI–Ts Relationship and the Transpiration from Sparse Vegetation in the Sahel Based on High-Resolution Satellite Data , 1999 .

[18]  S. Running,et al.  Developing Satellite-derived Estimates of Surface Moisture Status , 1993 .

[19]  Yann Kerr,et al.  IRSUTE: A Minisatellite Project for Land Surface Heat Flux Estimation from Field to Regional Scale , 1999 .

[20]  Y. Mitsuta Sino-Japanese Joint Research Project HEIFE : General View and Results , 2000 .

[21]  Estimating Regional Distribution of Sensible Heat Flux over Vegetation using Satellite Infrared Temp , 2000 .

[22]  Lei Shi,et al.  Surface Forcing of the Infrared Cooling Profile over the Tibetan Plateau. Part II: Cooling-Rate Variation over Large-Scale Plateau Domain during Summer Monsoon Transition , 1992 .

[23]  Bin Wang,et al.  Rainy Season of the Asian-Pacific Summer Monsoon(. , 2002 .

[24]  T. Fukuzono,et al.  The use of multi-temporal NOAA/AVHRR data to monitor surface moisture status in the Huaihe River Basin, China , 1998 .

[25]  T. Yamazaki,et al.  Evaluating the spatial and temporal distribution of snow accumulation, snowmelts and discharge in a multi basin scale: an application to the Tohoku Region, Japan , 2001 .

[26]  Rikie Suzuki,et al.  Relationships between meridional profiles of satellite-derived vegetation index (NDVI) and climate over Siberia , 2000 .

[27]  W. Dulaney,et al.  Normalized difference vegetation index measurements from the Advanced Very High Resolution Radiometer , 1991 .

[28]  J. Faundeen,et al.  The 1 km AVHRR global land data set: first stages in implementation , 1994 .

[29]  Garik Gutman,et al.  Vegetation indices from AVHRR: An update and future prospects , 1991 .

[30]  A. Higuchi,et al.  Analysis of Surface Moisture Status and Phenology in Thailand Using NOAA/AVHRR , 2001 .

[31]  Lei Shi,et al.  Surface Forcing of the Infrared Cooling Profile over the Tibetan Plateau. Part I: Influence of Relative Longwave Radiative Heating at High Altitude. , 1992 .

[32]  L. McMillin,et al.  Theory and validation of the multiple window sea surface temperature technique , 1984 .

[33]  K. Nishida,et al.  An Analysis of the Characteristics of NDVI-Radiative Temperature Relationship Aiming at to Estimate Latent Heat Flux at Regional Scale in the Tropical Monsoon Zone , 2000 .

[34]  G. Dedieu,et al.  Global-Scale Assessment of Vegetation Phenology Using NOAA/AVHRR Satellite Measurements , 1997 .

[35]  I. Sandholt,et al.  A simple interpretation of the surface temperature/vegetation index space for assessment of surface moisture status , 2002 .

[36]  C. Rao,et al.  Post-launch calibration of the visible and near-infrared channels of the Advanced Very High Resolution Radiometer on the NOAA-14 spacecraft , 1996 .

[37]  H. Yabuki,et al.  Seasonal change of land-surface processes in permafrost region of Tibetan Plateau , 1998 .

[38]  C. Tucker,et al.  Increased plant growth in the northern high latitudes from 1981 to 1991 , 1997, Nature.

[39]  S. Goward,et al.  Estimation of air temperature from remotely sensed surface observations , 1997 .

[40]  J. Estes,et al.  Applications of NOAA-AVHRR 1 km data for environmental monitoring , 1994 .

[41]  S. Goward,et al.  Evaluation of the NOAA/NASA Pathfinder AVHRR Land Data Set for global primary production , 1995 .

[42]  H. Jones,et al.  Plants and Microclimate. , 1985 .

[43]  S. Running,et al.  A continental phenology model for monitoring vegetation responses to interannual climatic variability , 1997 .

[44]  Nathaniel A. Brunsell,et al.  Scale issues in land-atmosphere interactions: implications for remote sensing of the surface energy balance , 2003 .

[45]  Richard K. Moore,et al.  Microwave Remote Sensing , 1999 .

[46]  Ramakrishna R. Nemani,et al.  Development of an evapotranspiration index from Aqua/MODIS for monitoring surface moisture status , 2003, IEEE Trans. Geosci. Remote. Sens..

[47]  Samuel N. Goward,et al.  Evaluating land surface moisture conditions from the remotely sensed temperature/vegetation index measurements: An exploration with the simplified simple biosphere model , 2002 .