a simple and novel algorithm for large-scale mapping of ... · 215.2 ×106 ha , (~9%) in africa,...

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A simple and novel algorithm for large-scale mapping of evergreen forests in tropical America, Africa and Asia Xiangming Xiao 1,2 , Chandrashekhar M. Biradar 1,2 , Christina Czarnecki 2 , Tunrayo Alabi 3 , and Michael Keller 2 1 Department of Botany and Microbiology, and Center for Spatial Analysis, University of Oklahoma, Norman, OK 73019, USA; 2 Institute for the Study of Earth, Oceans and Space, University of New Hampshire, Durham NH 03824, USA; 3 International Institute of Tropical Agriculture, Ibadan, Nigeria The areal extent and spatial distribution of evergreen forests in the tropical zone are important for the study of climate, carbon cycle and biodiversity. However, frequent cloud cover in the moist tropical region makes it a challenging task to map evergreen forests. In this study we developed a simple and novel mapping algorithm that is based on the temporal profile analysis of Land Surface Water Index (LSWI), which is calculated as a normalized ratio between near infrared and shortwave infrared spectral bands. The 8-day composites of MODIS Land Surface Reflectance data (MOD09A1) in 2001 at 500-m spatial resolution were used to calculate LSWI. The LSWI-based mapping algorithm was applied to map evergreen forests in tropical America, Africa and Asia (30 o N – 30 o S). The resultant evergreen forest map in 2001 (MOD100) was compared with ancillary data (FAO FRA), including other forest maps derived from more complex algorithms such as MOD12Q1 and GLC2000. (Friedl et al., 2002; Mayaux et al., 2006). INTRODUCTION MODIS land surface reflectance data and vegetation indices The MOD09A1 (2001, version 5) data were acquired from the USGS EROS Data Center (EDC; http://edc.usgs.gov ) and organized in a tile system with the Sinusoidal projection; datasets cover the tropical zone (ranging from 30 o N to 30 o S). For each MOD09A1 file, the quality of individual observations (e.g., clouds, cloud shadow) was identified, and three vegetation indices are calculated: MATERIALS & METHODS RESULTS & DISCUSSION CONCLUSIONS FAO (2001). Global Forest Resources Assessment 2000. In (p. 511). Rome, Italy: Food and Agriculture Organization of the United Nations Friedl, M.A., et al. (2002). Global land cover mapping from MODIS: algorithms and early results. Remote Sensing of Environment, 83, 287-302 Huete, A.R., et al (1997). A comparison of vegetation indices over a global set of TM images for EOS-MODIS. Remote Sensing of Environment, 59, 440-451 Tucker, C.J. (1979). Red and Photographic Infrared Linear Combinations for Monitoring Vegetation. Remote Sensing of Environment, 8, 127-150 Xiao, X., et al (2002a). Observation of flooding and rice transplanting of paddy rice fields at the site to landscape scales in China using VEGETATION sensor data. International Journal of Remote Sensing, 23, 3009-3022 Mayaux, P., et al, (2006). Validation of the global land cover 2000 map. IEEETransactions on Geoscience and Remote Sensing, 44, 1728- 1739 LITERATURE CITED This study was supported by NASA Interdisciplinary Science program (NAG5-10135, NNX07AH32G), NASA Terrestrial Ecology program (Large-scale Biosphere-Atmosphere Experiment in Amazon; NNG05GE28A), and NASA Land Use and Land Cover Change Program (NNX09AC39G). ACKNOWLEDGEMENT Normalized Difference Vegetation Index (NDVI) (Tucker 1979), Enhanced Vegetation Index (EVI) (Huete et al., 1997), and Land Surface Water Index (LSWI) (Xiao et al., 2002a), using Blue, Red, NIR1 (841–875 nm) and SWIR2 (1628–1652 nm) spectral bands. The vegetation indices data products are available to the public (http://www.eomf.ou.edu ). Temporal profile analysis for identifying and mapping evergreen forests --- leaf phenology-based approach A green leaf has higher NIR reflectance than SWIR reflectance, resulting in a LSWI value of above 0.0 (positive value). A senescent leaf and soils have lower NIR reflectance than SWIR reflectance, resulting in a LSWI value of below 0.0 (negative value). LSWI values of evergreen plants remain >0.0 for all good-quality observations throughout a year, while all the other land cover types have a number of observations with LSWI <0.0 values in a year (Figure 1). Based on this unique feature of LSWI time series data for evergreen plants, we developed a mapping algorithm to identify evergreen forest. The first step is to count number of good-quality observations that have LSWI values to be >0.0 in a year for a pixel. The second step is to assign a pixel that all of the good-quality observations have LSWI value of > 0.0 to be evergreen vegetation pixel. -0.2 -0.1 0.0 0.1 0.2 0.3 0.4 0.5 8 40 72 104 136 168 200 232 264 296 328 360 Land surface water index (LSWI) Day of year (8-day interval) in 2001 Evergreen forest Deciduous woodland Shrubland Cropland Fig. 1. The seasonal dynamics of Land Surface Water Index (LSWI) in 2001from six sites that represent major land-cover types in the tropical Africa. The evergreen forest site (20.9086 o E, 2.3042 o S) was located at the Salonga national park of Democratic Republic of Congo (IUCN/WWF (1985)); the deciduous woodland site (3.8437 o W, 9.4417 o N) at the Comoé National Park of Côte d'Ivoire; the savanna shrubland site (2.4341 o E, 11.7463 o N) at the Benin National Park of Republic of Benin (http://sea.unep-wcmc.org); the cropland site (8.3158 o E, 12.2098 o N) in Nigeria (selected from an IKONOS image of November 7, 2000); the savanna grassland site (30.4783 o E, 12.2829 o N) at the CO2 flux tower site in Demokeya, Sudan (http://www.fluxnet.ornl.gov/fluxnet); and the desert site (28.2478 o E, 18.2083 o N) in Sudan. red nir red nir ρ ρ ρ ρ NDVI + = 1 5 7 6 5 2 + × × + × = blue red nir red nir ρ . ρ ρ ρ ρ . EVI swir nir swir nir ρ ρ ρ ρ LSWI + = MOD100 MOD12Q1 Agreement Legend MOD100 MOD12Q1 Agreement Legend MOD100 MOD12Q1 Agreement Legend 0 100 200 300 400 500 600 700 800 America Africa Asia Tropical evergreen forest area (10 3 ha) FAO2000 GLC2000 MOD12Q1 MOD100 Evergreen forest area from MOD100 (10 3 ha) 0 20000 40000 60000 80000 360000 400000 Evergreen forest area from MOD12Q1 (10 3 ha) 0 20000 40000 60000 80000 360000 400000 Forest area by country 1:1 line Evergreen forest area from MOD100 (10 3 ha) 0 5000 10000 15000 20000 25000 120000 140000 Evergreen forest area from MOD12Q1 (10 3 ha) 0 5000 10000 15000 20000 25000 120000 140000 Forest area by country 1:1 line Evergreen forest area from MOD100 (10 3 ha) 0 10000 20000 30000 40000 50000 250000 Evergreen forest area from MOD12Q1 (10 3 ha) 0 10000 20000 30000 40000 50000 250000 Forest area by country 1:1 line The LSWI-based algorithm (the MOD100 dataset) estimates a total area of 709.7 ×10 6 ha evergreen forest in tropical Central and South America ~40.4% of the total land area 215.2 ×10 6 ha , (~9%) in Africa, and 233.7 ×10 6 ha (~ 14.5%) in Asia. In this paper, we reported a simple and novel algorithm for mapping evergreen forests in the tropical zone, and the advantage of the LSWI-based temporal profile analysis is that it does not require a large number of training datasets (including Landsat TM/ETM+ images), as it is based on leaf phenology. The LSWI-based algorithm was applied to quantify the area and spatial distribution of evergreen forests in 2001 in tropical America, Africa, and Asia, using the MODIS data at 500-m spatial resolution and 8-day temporal resolution in 2001. The areal extent and spatial distribution of evergreen forests in tropical Africa, America, and Asia from this LSWI- based mapping algorithm are similar to those of the standard MODIS Land Cover Product (MOD12Q1) that was generated from complex mapping algorithms (Friedl et al., 2002), although there are large discrepancies in Asia and Africa. The results from the inter-comparison of the four global forest datasets in the tropical zone suggested the potential of this LSWI-based mapping algorithm for identifying and mapping evergreen forests in the tropical zone. The implication of this study is that this LSWI-based mapping algorithm might be useful for operational monitoring of evergreen forests in the tropical world at moderate spatial resolution. Fig. 2. A comparison of evergreen forest areas in the tropical America, Africa and Asia (30 o N – 30 o S); (a) among the four global forest datasets (MOD100, MOD12Q1, GLC2000 and FAO FRA2000); A country-level comparison for the area estimates of evergreen forests between the LSWI-based algorithm in this study (MOD100) and the standard MODIS Land Cover Product (MOD12Q1) in 2001 for (b)America; (c) Africa and (d) Asia. Fig. 3. Spatial distribution of evergreen forests in tropical America, Africa and Asia (30 o N – 30 o S) in 2001 as estimated by the LSWI-based algorithm in this study (MOD100) in comparison to the MOD12Q1 dataset. In the figure legend, “Agreement” – evergreen forest pixels from both MOD100 and MOD12Q1; “MOD100” evergreen forest pixel from MOD100 only; “MOD12Q1” – evergreen forest pixels from MOD12Q1 only. America % Africa % Asia % World % MOD100 2446968 7 903025 6 2839807 14 6189800 9 MOD12Q1 3515233 10 4001688 28 3789844 18 11306765 16 Agreement 30617252 84 9295988 65 13961799 68 53875039 75 Total 36579453 100 14200701 100 20591450 100 71371604 100 Table 1. A summary of spatial comparison between MOD100 and MOD12Q1 datasets at the scale of continent and the entire tropical zone (30 o N - 30 o S) (a) (b) (c) (d) Contact us: [email protected] (Dr. Chandrashekhar Biradar) [email protected] (Dr. Xiangming Xiao)

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Page 1: A simple and novel algorithm for large-scale mapping of ... · 215.2 ×106 ha , (~9%) in Africa, and 233.7 ×106 ha (~ 14.5%) in Asia. In this paper, we reported a simple and novel

A simple and novel algorithm for large-scale mapping of evergreen forests in tropical America, Africa and AsiaXiangming Xiao1,2, Chandrashekhar M. Biradar1,2, Christina Czarnecki2, Tunrayo Alabi3, and Michael Keller2

1Department of Botany and Microbiology, and Center for Spatial Analysis, University of Oklahoma, Norman, OK 73019, USA; 2Institute for the Study of Earth, Oceans and Space, University of New Hampshire, Durham NH 03824, USA; 3International Institute of Tropical Agriculture, Ibadan, Nigeria

The areal extent and spatial distribution of evergreen forests inthe tropical zone are important for the study of climate, carboncycle and biodiversity. However, frequent cloud cover in themoist tropical region makes it a challenging task to mapevergreen forests. In this study we developed a simple andnovel mapping algorithm that is based on the temporal profileanalysis of Land Surface Water Index (LSWI), which iscalculated as a normalized ratio between near infrared andshortwave infrared spectral bands. The 8-day composites ofMODIS Land Surface Reflectance data (MOD09A1) in 2001 at500-m spatial resolution were used to calculate LSWI. TheLSWI-based mapping algorithm was applied to map evergreenforests in tropical America, Africa and Asia (30oN – 30oS).

The resultant evergreen forest map in 2001 (MOD100) was compared with ancillary data (FAO FRA), including other forest maps derived from more complex algorithms such as MOD12Q1 and GLC2000. (Friedl et al., 2002; Mayaux et al., 2006).

INTRODUCTION

MODIS land surface reflectance data and vegetation indices

The MOD09A1 (2001, version 5) data were acquired from theUSGS EROS Data Center (EDC; http://edc.usgs.gov) andorganized in a tile system with the Sinusoidal projection; datasetscover the tropical zone (ranging from 30oN to 30oS). For eachMOD09A1 file, the quality of individual observations (e.g., clouds,cloud shadow) was identified, and three vegetation indices arecalculated:

MATERIALS & METHODS

RESULTS & DISCUSSION CONCLUSIONS

FAO (2001). Global Forest Resources Assessment 2000. In (p. 511). Rome, Italy: Food and Agriculture Organization of the United Nations

Friedl, M.A., et al. (2002). Global land cover mapping from MODIS: algorithms and early results. Remote Sensing of Environment, 83, 287-302

Huete, A.R., et al (1997). A comparison of vegetation indices over a global set of TM images for EOS-MODIS. Remote Sensing of Environment, 59, 440-451

Tucker, C.J. (1979). Red and Photographic Infrared Linear Combinations for Monitoring Vegetation. Remote Sensing of Environment, 8, 127-150

Xiao, X., et al (2002a). Observation of flooding and rice transplanting of paddy rice fields at the site to landscape scales in China using VEGETATION sensor data. International Journal of Remote Sensing, 23, 3009-3022

Mayaux, P., et al, (2006). Validation of the global land cover 2000 map. IEEETransactions on Geoscience and Remote Sensing, 44, 1728-1739

LITERATURE CITED

This study was supported by NASA InterdisciplinaryScience program (NAG5-10135, NNX07AH32G),NASA Terrestrial Ecology program (Large-scaleBiosphere-Atmosphere Experiment in Amazon;NNG05GE28A), and NASA Land Use and LandCover Change Program (NNX09AC39G).

ACKNOWLEDGEMENT

Normalized Difference VegetationIndex (NDVI) (Tucker 1979),Enhanced Vegetation Index (EVI)(Huete et al., 1997), and LandSurface Water Index (LSWI) (Xiaoet al., 2002a), using Blue, Red,NIR1 (841–875 nm) and SWIR2(1628–1652 nm) spectral bands.The vegetation indices data products are available to the public (http://www.eomf.ou.edu ).

Temporal profile analysis for identifying and mapping evergreen forests --- leaf phenology-based approach

A green leaf has higher NIR reflectance than SWIR reflectance,resulting in a LSWI value of above 0.0 (positive value). Asenescent leaf and soils have lower NIR reflectance than SWIRreflectance, resulting in a LSWI value of below 0.0 (negativevalue). LSWI values of evergreen plants remain >0.0 for allgood-quality observations throughout a year, while all the otherland cover types have a number of observations with LSWI <0.0values in a year (Figure 1). Based on this unique feature of LSWItime series data for evergreen plants, we developed a mappingalgorithm to identify evergreen forest. The first step is to countnumber of good-quality observations that have LSWI values tobe >0.0 in a year for a pixel. The second step is to assign a pixelthat all of the good-quality observations have LSWI value of >0.0 to be evergreen vegetation pixel.

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Fig. 1. The seasonal dynamics of Land Surface Water Index (LSWI) in2001from six sites that represent major land-cover types in the tropicalAfrica. The evergreen forest site (20.9086oE, 2.3042oS) was located atthe Salonga national park of Democratic Republic of Congo (IUCN/WWF(1985)); the deciduous woodland site (3.8437oW, 9.4417oN) at the ComoéNational Park of Côte d'Ivoire; the savanna shrubland site (2.4341oE,11.7463oN) at the Benin National Park of Republic of Benin(http://sea.unep-wcmc.org); the cropland site (8.3158oE, 12.2098oN) inNigeria (selected from an IKONOS image of November 7, 2000); thesavanna grassland site (30.4783oE, 12.2829oN) at the CO2 flux tower sitein Demokeya, Sudan (http://www.fluxnet.ornl.gov/fluxnet); and the desertsite (28.2478oE, 18.2083oN) in Sudan.

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MOD100MOD12Q1Agreement

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The LSWI-based algorithm (the MOD100 dataset) estimatesa total area of 709.7 ×106 ha evergreen forest in tropicalCentral and South America ~40.4% of the total land area215.2 ×106 ha , (~9%) in Africa, and 233.7 ×106 ha (~14.5%) in Asia.

In this paper, we reported a simple and novel algorithm formapping evergreen forests in the tropical zone, and theadvantage of the LSWI-based temporal profile analysis is thatit does not require a large number of training datasets(including Landsat TM/ETM+ images), as it is based on leafphenology. The LSWI-based algorithm was applied to quantifythe area and spatial distribution of evergreen forests in 2001 intropical America, Africa, and Asia, using the MODIS data at500-m spatial resolution and 8-day temporal resolution in2001. The areal extent and spatial distribution of evergreenforests in tropical Africa, America, and Asia from this LSWI-based mapping algorithm are similar to those of the standardMODIS Land Cover Product (MOD12Q1) that was generatedfrom complex mapping algorithms (Friedl et al., 2002),although there are large discrepancies in Asia and Africa. Theresults from the inter-comparison of the four global forestdatasets in the tropical zone suggested the potential of thisLSWI-based mapping algorithm for identifying and mappingevergreen forests in the tropical zone. The implication of thisstudy is that this LSWI-based mapping algorithm might beuseful for operational monitoring of evergreen forests in thetropical world at moderate spatial resolution.

Fig. 2. A comparison of evergreen forest areas in the tropicalAmerica, Africa and Asia (30oN – 30oS); (a) among the four globalforest datasets (MOD100, MOD12Q1, GLC2000 and FAOFRA2000); A country-level comparison for the area estimates ofevergreen forests between the LSWI-based algorithm in this study(MOD100) and the standard MODIS Land Cover Product(MOD12Q1) in 2001 for (b)America; (c) Africa and (d) Asia.

Fig. 3. Spatial distribution of evergreen forests in tropical America, Africa andAsia (30oN – 30oS) in 2001 as estimated by the LSWI-based algorithm in thisstudy (MOD100) in comparison to the MOD12Q1 dataset. In the figurelegend, “Agreement” – evergreen forest pixels from both MOD100 andMOD12Q1; “MOD100” – evergreen forest pixel from MOD100 only;“MOD12Q1” – evergreen forest pixels from MOD12Q1 only.

America % Africa % Asia % World %MOD100 2446968 7 903025 6 2839807 14 6189800 9MOD12Q1 3515233 10 4001688 28 3789844 18 11306765 16Agreement 30617252 84 9295988 65 13961799 68 53875039 75Total 36579453 100 14200701 100 20591450 100 71371604 100

Table 1. A summary of spatial comparison between MOD100 and MOD12Q1 datasets at the scale of continent and the entire tropical zone (30oN - 30oS)

(a) (b)

(c) (d)

Contact us: [email protected] (Dr. Chandrashekhar Biradar)[email protected] (Dr. Xiangming Xiao)