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MODIS Collection 5 Land Cover Type and Land Cover Dynamics ... · data used to produce the MOD12...

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e The Moderate Resolution Imaging Spectroradiometer (MODIS) onboard NASA's Terra and Aqua spacecraft provides land surface data at global scales that are useful for a wide array of scientific applications related to land surface properties and processes. In the past year, land products from MODIS collection 5 reprocessing have become available. In this paper, we describe algorithm refinements and recent results from collection 5 reprocessing of the MODIS land cover type and land cover dynamics products (MOD12). Specifically, we summarize changes to the algorithms and data sets that are being used to characterize the geographic distribution and phenology of vegetation and land cover types at global scales. In collection 5, the MOD12 product is being produced at 500-meter spatial resolution using 8-day inputs from the MODIS normalized BRDF-adjusted (NBAR) product. The increased spatial and temporal resolution of the input data used to produce the MOD12 product represent significant steps forward and result in substantial improvements relative to the MOD12 collection 4 products. This poster describes specific changes to algorithms and input data that are being used in collection 5, and will provide preliminary assessments regarding changes in product quality. Abstract Preliminary Results for Land Cover Type MODIS Collection 5 Land Cover Type and Land Cover Dynamics: Algorithm Refinements and Early Assessment Damien Sulla-Menashe and Mark Frield Department of Geography and Environment, Boston University, 675 Commonwealth Avenue, Boston, MA 02215 http://www. bu . edu/geography Refinements to the STEP database Algorithm Refinements The System for Terrestrial Ecosystem Parameterization (STEP) database provides training data for the MOD12Q1 land cover type product algorithm. In preparation for collection 5 the STEP database was analyzed and extensively revised to insure representative sampling of land cover. Specifically, we examined: o Geographic & ecological sampling based on biogeographic realms, global biomes from Olson et al. (2001), and country level statistics. o Outlier and error analysis based on PCA of raw NBAR data, annual EVI profiles, and measures of internal heterogeneity. o The distribution and sampling of agricultural sites using crop inventory data. Results from these analyses lead to the following changes to the STEP database: o Addition of wetland and forest sites in China; deciduous needleleaf sites in Siberia; forest sites in New Zealand; and agricultural sites in Sahelian Africa, Mexico, India, Canada, and New Zealand. o Reduction in size or removal of large sites such (e.g., large snow/ice sites in Greenland). o Re-labeling or removal of sites based on new sources of data including ancillary maps, high resolution imagery, or EVI temporal profiles. o Removal of sites that were internally heterogeneous, or mixed. Ancillary data layers are used within the MOD12Q1 algorithm to aid classification results when data from MODIS do not effectively separate classes. These data are derived from a variety of sources including the Collection 4 MOD12Q1 product, agricultural intensity data, and the MODIS land water mask. A 150 km x 150 km moving window was used to compute the approximate regional frequency of classes based on MODIS collection 4 data; this provides local likelihoods for each class at each pixel. To prescribe the likelihood of agriculture or agricultural mosaic, we used a new data set from Ramankutty et al. (2008, in press, GBC; see below). The Collection 5 MOD12 product will include a number significant changes and refinements. Most importantly, the C5 product will be based on input data with increased spatial and temporal resolution. In the case of land cover type, the algorithm now uses land surface temperature in addition to surface reflectance. These improvements increase the overall quality of the product by: (1) providing a more accurate representation of vegetation patterns at sub-kilometer scales, (2) through improved quality and frequency of measurements in areas of persistent cloud cover, and (3) by reducing misclassification due to mixed pixels and missing data. The most important of these changes are summarized in the table below. •Updated to more recent (2000+) imagery •Updated to conform to require-ments for 500-m data •Extensive quality control including editing and removal of bad sites •Augmentation of sites in under- represented areas and classes •Largely based on older TM5 data •Large sites with significant internal heterogeneity. •Inadequate quality control •Relatively poor and misrepresentative sampling in key areas STEP Database Major Changes to the MOD12 Land Cover Type and Land Cover Dynamics Products (MOD12Q1, MOD12Q2) •Decreased reliance (weighting) on prior probability layers •Improved treatment/representation of deciduous needleleaf forests •Improved treatment/representation of wetlands •Improved gap filling and screening for snow •Significant reliance on out-of-date prior probability layers •Ad hoc reduction of overestimated deciduous needleleaf forests and wetlands •Ad hoc screening for snow and gap filling for missing data Algorithms •MODIS V5 land-water mask •Updated V5 urban layer •Prior probability layers based on Collection 4 data with inclusion of new agricultural intensity data •MODIS V4 land-water mask •V4 urban mask •Prior probability layers based on Collection 3 data and ancillary data related global croplands intensity Ancillary Data •32-day NBAR (7 land bands), EVI and LST data at 500-m resolution derived from four 8-day values. •Annual metrics (min, max, mean) for each of the above bands. •8-day EVI computed from NBAR data •32-day NBAR data (7 land bands) at 1-km resolution derived from two 16-day values. •32-Day EVI data at 1-km •Annual metrics (min, max, mean) for each of the above bands. •16-day EVI computed from NBAR data Inputs V5 V4 Below: Cropland intensity (Ramankutty et al ); Above right: probability of > 60% croplands; Below right: probability of agricultural mosaic. Improved characterization of high latitude vegetation extending to the Arctic Ocean Delta of the Kolyma River, Eastern Siberia Improved representation and detection of wetland ecosystems. Hudson Bay lowlands wetland complex Improved ancillary information results in a better depiction of agriculture in Africa Croplands on Western shores of Lake Victoria Higher spatial resolution clarifies areas of forest degradation and loss Deforestation in Brazil, state of Para IGBP Class Distribution in the STEP Database 0 50 100 150 200 250 300 350 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 IGBP Class Frequency Collection 5 Refinements to the Land Cover Dynamics Product Refinements to the collection 5 land cover dynamics product (MOD12Q2) include changes to the algorithm and input data. Most importantly, 500-m NBAR data at 8-day intervals are being used to model land cover dynamics on seasonal time scales (phenology). As a result, the spatial resolution of the product has increased from 1-km to 500-m, and detection of phenological transition dates should be both more accurate. In addition, the algorithm used to produce collection 5 results includes a number of subtle changes that affect how missing data in NBAR data are treated, and how snow is both detected and accounted for in the algorithm (see below). Snow info for tile h12v04 of day 81 and 97 in 2002. The left column is the snow flag provided with MODIS NBAR product. The middle and right columns are spatially aggregated MOD10A2 with majority and conservative methods, respectively. In the majority method, a 16-day 1-km pixel is marked as snow if the more than 50% of the 8-day 500-m pixels are marked as snow in MOD10A2. In the conservative method, a 16-day 1-km pixel is marked as snow if any 8-day 500-m pixels are marked as snow in MOD10A2. Snow Non- Snow Cloud Fill Majority Method Conservative Method Day 81 Day 97 NBAR snow flag This work was supported by NASA grant # NNG04HZ71C. We also gratefully acknowledge the many contributions by numerous individuals in recent years, especially Dr. Bin Tan and Dr. Xiaoyang Zhang, both of whom were instrumental in implementing and refining the MOD12 algorithms Updated Ancillary Data Layers Acknowledgements Global Class Distribution 0 2 4 6 8 10 12 14 16 18 20 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 Percent Land Area V4 V5 North America Class Distribution V4 V5 South America Class Distribution V4 V5 Eurasia Class Distribution V4 V5 Africa Class Distribution V4 V5 Oceania Class Distribution V4 V5
Transcript
Page 1: MODIS Collection 5 Land Cover Type and Land Cover Dynamics ... · data used to produce the MOD12 product represent significant steps forward and result in substantial improvements

e

The Moderate Resolution Imaging Spectroradiometer (MODIS) onboardNASA's Terra and Aqua spacecraft provides land surface data at globalscales that are useful for a wide array of scientific applications related to landsurface properties and processes. In the past year, land products fromMODIS collection 5 reprocessing have become available. In this paper, wedescribe algorithm refinements and recent results from collection 5reprocessing of the MODIS land cover type and land cover dynamicsproducts (MOD12). Specifically, we summarize changes to the algorithmsand data sets that are being used to characterize the geographic distributionand phenology of vegetation and land cover types at global scales. Incollection 5, the MOD12 product is being produced at 500-meter spatialresolution using 8-day inputs from the MODIS normalized BRDF-adjusted(NBAR) product. The increased spatial and temporal resolution of the inputdata used to produce the MOD12 product represent significant steps forwardand result in substantial improvements relative to the MOD12 collection 4products. This poster describes specific changes to algorithms and input datathat are being used in collection 5, and will provide preliminary assessmentsregarding changes in product quality.

Abstract Preliminary Results for Land Cover Type(MOD12Q1)

MODIS Collection 5 Land Cover Type and Land Cover Dynamics: AlgorithmRefinements and Early AssessmentDamien Sulla-Menashe and Mark FrieldDepartment of Geography and Environment, Boston University, 675 Commonwealth Avenue, Boston, MA 02215http://www.bu.edu/geography

Refinements to the STEP database

Algorithm Refinements

• The System for Terrestrial Ecosystem Parameterization (STEP) database provides trainingdata for the MOD12Q1 land cover type product algorithm.

• In preparation for collection 5 the STEP database was analyzed and extensively revised toinsure representative sampling of land cover. Specifically, we examined:oGeographic & ecological sampling based on biogeographic realms, global biomes from

Olson et al. (2001), and country level statistics.oOutlier and error analysis based on PCA of raw NBAR data, annual EVI profiles, and

measures of internal heterogeneity.o The distribution and sampling of agricultural sites using crop inventory data.

• Results from these analyses lead to the following changes to the STEP database:oAddition of wetland and forest sites in China; deciduous needleleaf sites in Siberia; forest

sites in New Zealand; and agricultural sites in Sahelian Africa, Mexico, India, Canada,and New Zealand.

oReduction in size or removal of large sites such (e.g., large snow/ice sites in Greenland).oRe-labeling or removal of sites based on new sources of data including ancillary maps,

high resolution imagery, or EVI temporal profiles.oRemoval of sites that were internally heterogeneous, or mixed.

• Ancillary data layers are used within the MOD12Q1 algorithm to aidclassification results when data from MODIS do not effectively separateclasses. These data are derived from a variety of sources including theCollection 4 MOD12Q1 product, agricultural intensity data, and the MODISland water mask.

• A 150 km x 150 km moving window was used to compute the approximateregional frequency of classes based on MODIS collection 4 data; thisprovides local likelihoods for each class at each pixel.

• To prescribe the likelihood of agriculture or agricultural mosaic, we used anew data set from Ramankutty et al. (2008, in press, GBC; see below).

The Collection 5 MOD12 product will include a number significant changesand refinements. Most importantly, the C5 product will be based on inputdata with increased spatial and temporal resolution. In the case of land covertype, the algorithm now uses land surface temperature in addition to surfacereflectance. These improvements increase the overall quality of the productby: (1) providing a more accurate representation of vegetation patterns atsub-kilometer scales, (2) through improved quality and frequency ofmeasurements in areas of persistent cloud cover, and (3) by reducingmisclassification due to mixed pixels and missing data. The most important ofthese changes are summarized in the table below.

•Updated to more recent (2000+) imagery•Updated to conform to require-ments for500-m data•Extensive quality control includingediting and removal of bad sites•Augmentation of sites in under-represented areas and classes

•Largely based on older TM5 data•Large sites with significant internalheterogeneity.•Inadequate quality control•Relatively poor and misrepresentativesampling in key areas

STEPDatabase

Major Changes to the MOD12 Land Cover Type and Land Cover Dynamics Products (MOD12Q1,MOD12Q2)

•Decreased reliance (weighting) on priorprobability layers•Improved treatment/representation ofdeciduous needleleaf forests•Improved treatment/representation ofwetlands•Improved gap filling and screening forsnow

•Significant reliance on out-of-date priorprobability layers•Ad hoc reduction of overestimateddeciduous needleleaf forests and wetlands•Ad hoc screening for snow and gap fillingfor missing data

Algorithms

•MODIS V5 land-water mask•Updated V5 urban layer•Prior probability layers based onCollection 4 data with inclusion of newagricultural intensity data

•MODIS V4 land-water mask•V4 urban mask•Prior probability layers based on Collection3 data and ancillary data related globalcroplands intensity

Ancillary Data

•32-day NBAR (7 land bands), EVI andLST data at 500-m resolution derivedfrom four 8-day values.•Annual metrics (min, max, mean) foreach of the above bands.•8-day EVI computed from NBAR data

•32-day NBAR data (7 land bands) at 1-kmresolution derived from two 16-day values.•32-Day EVI data at 1-km•Annual metrics (min, max, mean) for eachof the above bands.•16-day EVI computed from NBAR data

Inputs

V5V4

Below: Cropland intensity (Ramankutty et al );Above right: probability of > 60% croplands;

Below right: probability of agricultural mosaic.

Improvedcharacterization of

high latitudevegetation extendingto the Arctic Ocean

Delta of the Kolyma River, Eastern Siberia

Improvedrepresentation anddetection of wetland

ecosystems.

Hudson Bay lowlands wetland complex

Improved ancillaryinformation results in a

better depiction ofagriculture in Africa

Croplands on Western shores of Lake Victoria

Higher spatialresolution clarifies areas

of forest degradationand loss

Deforestation in Brazil, state of Para

IGBP Class Distribution in the STEP Database

0

50

100

150

200

250

300

350

1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17

IGBP Class

Fre

qu

en

cy

Collection 5 Refinements to the LandCover Dynamics Product

Refinements to the collection 5 land cover dynamics product (MOD12Q2)include changes to the algorithm and input data. Most importantly, 500-mNBAR data at 8-day intervals are being used to model land cover dynamics onseasonal time scales (phenology). As a result, the spatial resolution of theproduct has increased from 1-km to 500-m, and detection of phenologicaltransition dates should be both more accurate. In addition, the algorithm usedto produce collection 5 results includes a number of subtle changes that affecthow missing data in NBAR data are treated, and how snow is both detectedand accounted for in the algorithm (see below).

Snow info for tile h12v04 of day 81 and 97 in 2002. The left column is thesnow flag provided with MODIS NBAR product. The middle and rightcolumns are spatially aggregated MOD10A2 with majority and conservativemethods, respectively. In the majority method, a 16-day 1-km pixel is markedas snow if the more than 50% of the 8-day 500-m pixels are marked as snow inMOD10A2. In the conservative method, a 16-day 1-km pixel is marked assnow if any 8-day 500-m pixels are marked as snow in MOD10A2.

Snow

Non-Snow

Cloud

Fill

Majority Method Conservative Method

Day 81

Day 97

NBAR snow flag

This work was supported by NASA grant # NNG04HZ71C. We also gratefullyacknowledge the many contributions by numerous individuals in recent years,especially Dr. Bin Tan and Dr. Xiaoyang Zhang, both of whom wereinstrumental in implementing and refining the MOD12 algorithms

Updated Ancillary Data Layers

Acknowledgements

Global Class Distribution

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8

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18

20

1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16

Percen

t L

an

d A

rea

V4 V5

North America Class Distribution

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d A

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V4 V5

South America Class Distribution

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45

1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16

Pe

rc

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d A

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a

V4 V5

Eurasia Class Distribution

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1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16

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V4 V5

Africa Class Distribution

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Pe

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V4 V5

Oceania Class Distribution

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Pe

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V4 V5

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