Evaluation of the Quality of NDVI3g Dataset against Collection 6 MODIS NDVI in Central Europe between 2000 and 2013

Remote sensing provides invaluable insight into the dynamics of vegetation with global coverage and reasonable temporal resolution. Normalized Difference Vegetation Index (NDVI) is widely used to study vegetation greenness, production, phenology and the responses of ecosystems to climate fluctuations. The extended global NDVI3g dataset created by Global Inventory Modeling and Mapping Studies (GIMMS) has an exceptional 32 years temporal coverage. Due to the methodology that was used to create NDVI3g inherent noise and uncertainty is present in the dataset. To evaluate the accuracy and uncertainty of application of NDVI3g at regional scale we used Collection-6 data from the MODerate resolution Imaging Spectroradiometer (MODIS) sensor on board satellite Terra as a reference. After noise filtering, statistical harmonization of the NDVI3g dataset was performed for Central Europe based on MOD13 NDVI. Mean seasonal NDVI profiles, start, end and length of the growing season, magnitude and timing of peak NDVI were calculated from NDVI3g (original, noise filtered and harmonized) and MODIS NDVI and compared with each other. NDVI anomalies were also compared and evaluated using simple climate sensitivity metrics. The results showed that (1) the original NDVI3g has limited applicability in Central Europe, which was also implied by the significant disagreement between the NDVI3g and MODIS NDVI datasets; (2) the harmonization of NDVI3g with MODIS NDVI is promising since the newly created dataset showed improved quality for diverse vegetation metrics. For NDVI anomaly detection NDVI3g showed limited applicability, even after harmonization. Climate–NDVI relationships are not represented well by NDVI3g. The presented results can help researchers to assess the expected quality of the NDVI3g-based studies in Central Europe.

[1]  O. Sonnentag,et al.  Climate change, phenology, and phenological control of vegetation feedbacks to the climate system , 2013 .

[2]  Yujie Wang,et al.  Scientific Impact of MODIS C5 Calibration Degradation and C6+ Improvements , 2014 .

[3]  Rasmus Fensholt,et al.  Global-scale mapping of changes in ecosystem functioning from earth observation-based trends in total and recurrent vegetation , 2015 .

[4]  B. Holben Characteristics of maximum-value composite images from temporal AVHRR data , 1986 .

[5]  Berrien Moore,et al.  The response of global terrestrial ecosystems to interannual temperature variability , 1997 .

[6]  Francisco Javier García-Haro,et al.  Conventional and fuzzy comparisons of large scale land cover products: Application to CORINE, GLC2000, MODIS and GlobCover in Europe , 2012 .

[7]  Compton J. Tucker,et al.  A Non-Stationary 1981-2012 AVHRR NDVI3g Time Series , 2014, Remote. Sens..

[8]  S. Dech,et al.  The relationship between precipitation anomalies and satellite-derived vegetation activity in Central Asia , 2013 .

[9]  T. Udelhoven,et al.  Assessment of rainfall and NDVI anomalies in Spain (1989–1999) using distributed lag models , 2009 .

[10]  Patrick Minnis,et al.  The calibration of AVHRR visible dual gain using Meteosat-8 for NOAA-16 to 18 , 2007, SPIE Optical Engineering + Applications.

[11]  Ramakrishna R. Nemani,et al.  A generalized, bioclimatic index to predict foliar phenology in response to climate , 2004 .

[12]  P. Ciais,et al.  Unexpected role of winter precipitation in determining heat requirement for spring vegetation green‐up at northern middle and high latitudes , 2014, Global change biology.

[13]  D. Morton,et al.  Impact of sensor degradation on the MODIS NDVI time series , 2012 .

[14]  Gao Hao,et al.  Assessing MODIS Land Cover Products over China with Probability of Interannual Change , 2014 .

[15]  Arthur P. Cracknell,et al.  The exciting and totally unanticipated success of the AVHRR in applications for which it was never intended , 2001 .

[16]  Natascha Kljun,et al.  Spatial representativeness of tall tower eddy covariance measurements using remote sensing and footprint analysis. , 2009 .

[17]  Andrew D Richardson,et al.  The timing of autumn senescence is affected by the timing of spring phenology: implications for predictive models , 2015, Global change biology.

[18]  M. Shen,et al.  Precipitation impacts on vegetation spring phenology on the Tibetan Plateau , 2015, Global change biology.

[19]  Rasmus Fensholt,et al.  Evaluating MODIS, MERIS, and VEGETATION vegetation indices using in situ measurements in a semiarid environment , 2006, IEEE Transactions on Geoscience and Remote Sensing.

[20]  A. Huete,et al.  Overview of the radiometric and biophysical performance of the MODIS vegetation indices , 2002 .

[21]  I. Wing,et al.  Net carbon uptake has increased through warming-induced changes in temperate forest phenology , 2014 .

[22]  Clement Atzberger,et al.  Phenological Metrics Derived over the European Continent from NDVI3g Data and MODIS Time Series , 2013, Remote. Sens..

[23]  Xuhui Zhou,et al.  Similar responses of soil carbon storage to drought and irrigation in terrestrial ecosystems but with contrasting mechanisms: A meta-analysis , 2016 .

[24]  M. Marshall,et al.  Global assessment of Vegetation Index and Phenology Lab (VIP) and Global Inventory Modeling and Mapping Studies (GIMMS) version 3 products , 2015 .

[25]  Bernhard Schölkopf,et al.  A few extreme events dominate global interannual variability in gross primary production , 2014 .

[26]  Serge Rambal,et al.  Evaluation of the potential of MODIS satellite data to predict vegetation phenology in different biomes: An investigation using ground-based NDVI measurements , 2013 .

[27]  Shunlin Liang,et al.  Time‐lag effects of global vegetation responses to climate change , 2015, Global change biology.

[28]  Y. Hong,et al.  Vegetation Greening and Climate Change Promote Multidecadal Rises of Global Land Evapotranspiration , 2015, Scientific Reports.

[29]  Xiangming Xiao,et al.  Spatial analysis of growing season length control over net ecosystem exchange , 2005 .

[30]  Marc Macias-Fauria,et al.  Sensitivity of global terrestrial ecosystems to climate variability , 2016, Nature.

[31]  Tilden P. Meyers,et al.  Determining vegetation indices from solar and photosynthetically active radiation fluxes , 2007 .

[32]  Edwin W. Pak,et al.  An extended AVHRR 8‐km NDVI dataset compatible with MODIS and SPOT vegetation NDVI data , 2005 .

[33]  Tim R. McVicar,et al.  Global evaluation of four AVHRR-NDVI data sets: Intercomparison and assessment against Landsat imagery , 2011 .

[34]  Jennifer N. Hird,et al.  Noise reduction of NDVI time series: An empirical comparison of selected techniques , 2009 .

[35]  J. D. Tarpley,et al.  Global vegetation indices from the NOAA-7 meteorological satellite , 1984 .

[36]  Siham Tabik,et al.  Evaluating the Consistency of the 1982–1999 NDVI Trends in the Iberian Peninsula across Four Time-series Derived from the AVHRR Sensor: LTDR, GIMMS, FASIR, and PAL-II , 2010, Sensors.

[37]  P. Ciais,et al.  Influence of spring and autumn phenological transitions on forest ecosystem productivity , 2010, Philosophical Transactions of the Royal Society B: Biological Sciences.

[38]  Hongyan Liu,et al.  Trends toward an earlier peak of the growing season in Northern Hemisphere mid‐latitudes , 2016, Global change biology.

[39]  Laurent Tits,et al.  A model quantifying global vegetation resistance and resilience to short‐term climate anomalies and their relationship with vegetation cover , 2015 .

[40]  Nuno Carvalhais,et al.  Codominant water control on global interannual variability and trends in land surface phenology and greenness , 2015, Global change biology.

[41]  S. Bruin,et al.  Analysis of monotonic greening and browning trends from global NDVI time-series , 2011 .

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

[43]  Jorge E. Pinzón,et al.  Evaluating and Quantifying the Climate-Driven Interannual Variability in Global Inventory Modeling and Mapping Studies (GIMMS) Normalized Difference Vegetation Index (NDVI3g) at Global Scales , 2013, Remote. Sens..

[44]  A. Belward,et al.  The Best Index Slope Extraction ( BISE): A method for reducing noise in NDVI time-series , 1992 .

[45]  Alan H. Strahler,et al.  The Moderate Resolution Imaging Spectroradiometer (MODIS): land remote sensing for global change research , 1998, IEEE Trans. Geosci. Remote. Sens..

[46]  A. Jarvis Hole-field seamless SRTM data, International Centre for Tropical Agriculture (CIAT) , 2008 .

[47]  Stuart E. Marsh,et al.  Multi-sensor NDVI data continuity: Uncertainties and implications for vegetation monitoring applications , 2006 .

[48]  Xiaoxiong Xiong,et al.  Overview of NASA Earth Observing Systems Terra and Aqua moderate resolution imaging spectroradiometer instrument calibration algorithms and on-orbit performance , 2009 .

[49]  S. Kalluri,et al.  The Pathfinder AVHRR land data set: An improved coarse resolution data set for terrestrial monitoring , 1994 .

[50]  S. Garrigues,et al.  Multiscale geostatistical analysis of AVHRR, SPOT-VGT, and MODIS global NDVI products , 2008 .

[51]  Sietse O. Los,et al.  Response of vegetation to the 2003 European drought was mitigated by height , 2013 .

[52]  J. Bartholy,et al.  Bridging the gap between climate models and impact studies: the FORESEE Database , 2015, Geoscience data journal.

[53]  Benjamin F. Zaitchik,et al.  Europe's 2003 heat wave: a satellite view of impacts and land–atmosphere feedbacks , 2006 .

[54]  Konstantin V. Khlopenkov,et al.  Generating historical AVHRR 1 km baseline satellite data records over Canada suitable for climate change studies , 2005 .

[55]  P. Ciais,et al.  Europe-wide reduction in primary productivity caused by the heat and drought in 2003 , 2005, Nature.

[56]  David P. Roy,et al.  Generating a long-term land data record from the AVHRR and MODIS Instruments , 2007, 2007 IEEE International Geoscience and Remote Sensing Symposium.

[57]  Molly E. Brown,et al.  Evaluation of the consistency of long-term NDVI time series derived from AVHRR,SPOT-vegetation, SeaWiFS, MODIS, and Landsat ETM+ sensors , 2006, IEEE Transactions on Geoscience and Remote Sensing.

[58]  Anita Simic Milas,et al.  Assessment of Forest Damage in Croatia using Landsat-8 OLI Images , 2015 .

[59]  P. Atkinson,et al.  Amazon vegetation greenness as measured by satellite sensors over the last decade , 2011 .

[60]  Atul K. Jain,et al.  The dominant role of semi-arid ecosystems in the trend and variability of the land CO2 sink , 2015, Science.

[61]  R. Stöckli,et al.  European plant phenology and climate as seen in a 20-year AVHRR land-surface parameter dataset , 2004 .

[62]  Pierre Friedlingstein,et al.  Carbon–climate feedbacks: a review of model and observation based estimates , 2010 .

[63]  S. Bruin,et al.  Trend changes in global greening and browning: contribution of short‐term trends to longer‐term change , 2012 .

[64]  J. Peñuelas,et al.  Matching the phenology of Net Ecosystem Exchange and vegetation indices estimated with MODIS and FLUXNET in-situ observations , 2016 .

[65]  R. Fensholt,et al.  Evaluation of Earth Observation based global long term vegetation trends — Comparing GIMMS and MODIS global NDVI time series , 2012 .

[66]  T. Vesala,et al.  Reduction of ecosystem productivity and respiration during the European summer 2003 climate anomaly: a joint flux tower, remote sensing and modelling analysis , 2007 .

[67]  A. Wu,et al.  Assessing the consistency of AVHRR and MODIS L1B reflectance for generating Fundamental Climate Data Records , 2008 .

[68]  C. Tucker,et al.  A Global 9-yr Biophysical Land Surface Dataset from NOAA AVHRR Data , 2000 .

[69]  Ling Luo,et al.  Integrating AVHRR and MODIS data to monitor NDVI changes and their relationships with climatic parameters in Northeast China , 2012, Int. J. Appl. Earth Obs. Geoinformation.

[70]  Shilong Piao,et al.  Temperature, precipitation, and insolation effects on autumn vegetation phenology in temperate China , 2016, Global change biology.

[71]  Mark A. Friedl,et al.  Global vegetation phenology from Moderate Resolution Imaging Spectroradiometer (MODIS): Evaluation of global patterns and comparison with in situ measurements , 2006 .

[72]  P. Ciais,et al.  Spatiotemporal patterns of terrestrial carbon cycle during the 20th century , 2009 .

[73]  Philippe Ciais,et al.  Growing season extension and its impact on terrestrial carbon cycle in the Northern Hemisphere over the past 2 decades , 2007 .

[74]  Kamel Didan didan MULTI-SATELLITE EARTH SCIENCE DATA RECORD FOR STUDYING GLOBAL VEGETATION TRENDS AND CHANGES , 2009 .

[75]  Nadine Unger,et al.  Probing the past 30-year phenology trend of US deciduous forests , 2015 .

[76]  P. A. Schultz,et al.  Global correlation of temperature, NDVI and precipitation , 1993 .

[77]  Rogier de Jong,et al.  Variability and evolution of global land surface phenology over the past three decades (1982–2012) , 2016, Global change biology.

[78]  Jan Verbesselt,et al.  Trend Change Detection in NDVI Time Series: Effects of Inter-Annual Variability and Methodology , 2013, Remote. Sens..

[79]  C. Justice,et al.  A global 1° by 1° NDVI data set for climate studies derived from the GIMMS continental NDVI data , 1994 .

[80]  Florian Detsch,et al.  A Comparative Study of Cross-Product NDVI Dynamics in the Kilimanjaro Region - A Matter of Sensor, Degradation Calibration, and Significance , 2016, Remote. Sens..

[81]  R. Schnur,et al.  Climate-carbon cycle feedback analysis: Results from the C , 2006 .

[82]  A. Strahler,et al.  Monitoring vegetation phenology using MODIS , 2003 .

[83]  Nan Jiang,et al.  A Comparative Analysis between GIMSS NDVIg and NDVI3g for Monitoring Vegetation Activity Change in the Northern Hemisphere during 1982-2008 , 2013, Remote. Sens..

[84]  P. Jones,et al.  A European daily high-resolution gridded data set of surface temperature and precipitation for 1950-2006 , 2008 .

[85]  Damien Sulla-Menashe,et al.  MODIS Collection 5 global land cover: Algorithm refinements and characterization of new datasets , 2010 .

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

[87]  Shilong Piao,et al.  Delayed autumn phenology in the Northern Hemisphere is related to change in both climate and spring phenology , 2016, Global change biology.

[88]  Laura Dobor,et al.  Future climate of the Carpathians: climate change hot-spots and implications for ecosystems , 2016, Regional Environmental Change.

[89]  T. Sakamoto,et al.  A crop phenology detection method using time-series MODIS data , 2005 .

[90]  S. Ganguly,et al.  Amazon forests did not green‐up during the 2005 drought , 2009 .

[91]  Jinwei Dong,et al.  Green-up dates in the Tibetan Plateau have continuously advanced from 1982 to 2011 , 2013, Proceedings of the National Academy of Sciences.

[92]  D. Basler Evaluating phenological models for the prediction of leaf-out dates in six temperate tree species across central Europe , 2016 .

[93]  J. A. Schell,et al.  Monitoring vegetation systems in the great plains with ERTS , 1973 .

[94]  Martin Herold,et al.  Some challenges in global land cover mapping : An assessment of agreement and accuracy in existing 1 km datasets , 2008 .