(1) The study estimated the above-ground biomass of Milanchowk Community Forest in Nepal using field inventory data and satellite imagery. (2) A regression model was developed between above-ground biomass measured in 20 sample plots and vegetation indices derived from a Sentinel 2 image. (3) The maximum, minimum and average biomass estimates from the sample plots were 2164 kg, 422 kg and 1263 kg respectively. The regression model was validated and found to accurately estimate biomass across 10 additional plots.
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Digital Elevation Model (DEM) is the digital representation of the land surface elevation with respect to any reference datum. DEM is frequently used to refer to any digital representation of a topographic surface. DEM is the simplest form of digital representation of topography. GIS applications depend mainly on DEMs, today.
Application of remote sensing in forest ecosystemaliya nasir
Established remote sensing systems provide opportunities to develop and apply new measurements of ecosystem function across landscapes, regions and continents.
New efforts to predict the consequences of ecosystem function change, both natural and human- induced, on the regional and global distributions and abundances of species should be a high research priority
Making FCC Erdas from AWiFS/LISS-III individual bands dataSonal Aggarwal
This presentation shows how to make False Color composite (FCC) in Erdas from AWiFS/LISS-III individual bands data. AWiFS/LISS-III data can be obtained through NRSC Open EO Data Archive (NOEDA) in Bhuvan website.
Digital Elevation Model (DEM) is the digital representation of the land surface elevation with respect to any reference datum. DEM is frequently used to refer to any digital representation of a topographic surface. DEM is the simplest form of digital representation of topography. GIS applications depend mainly on DEMs, today.
Application of remote sensing in forest ecosystemaliya nasir
Established remote sensing systems provide opportunities to develop and apply new measurements of ecosystem function across landscapes, regions and continents.
New efforts to predict the consequences of ecosystem function change, both natural and human- induced, on the regional and global distributions and abundances of species should be a high research priority
To meet the various information requirements in forest management, different data sources like field survey, aerial photography, and satellite imagery is used, depending on the level of detail required and the extension of the area under study.
Remote Sensing Data Acquisition,Scanning/Imaging systemsdaniyal rustam
full of concepts about RS data acquisition scanning and imaging systems. Best for students of remote sensing. in this presentation we briefly explained the concept of scanning in remote sensing.
hyperspectral remote sensing and its geological applicationsabhijeet_banerjee
this is an introductory presentation on hyperspectral remote sensing, which essential deals with the distinguishing features, imaging spectrometers and its types, and some of the geological applications of hyperspectral remote sensing.
This document help you to prepare Triangulation Network (TIN), Hillshade Map, Slope map, interpolation and Digital Elevation Model (DEM) in a area and how to interpret them.
A remote sensing system uses a detector to sense the reflected or emitted energy from the earth's surface, perhaps modified by the intervening atmosphere. The sensor can be on a satellite, aircraft, or drone. The sensor turns the energy into a voltage, which an analog to digital converter turns into a single integer value (called the Digital Number, or DN) for the energy. Alternatively a digital detector can store the DN directly. We can then display this value with an appropriate color to build up an image of the region sensed by the system. The DN represents the energy sensed by the sensor in a particular part of the electromagnetic spectrum, emitted or reflected from a particular region. The principles can also be applied to sonar imagery, especially useful in water where sound penetrates readily whereas electromagnetic energy attenuates rapidly.
Definitions,
Remote sensing systems can be active or passive: active systems put out their own source of energy (a large "flash bulb") whereas passive systems use solar energy reflected from the surface or thermal energy emitted by the surface. Active systems can achieve higher resolution.
Satellite resolution considers four things: spatial, spectral, radiometric, and temporal resolution.
Electromagnetic radiation and the atmosphere control many aspects of a remote sensing system.
Satellite orbits determine many characteristics of the imagery, what the satellite sees, and how often it revisits an area.
The signal to noise ratio is important for the design of remote sensing systems.
Satellite band tradeoffs.
Interpreting satellite reflectance patterns and images uses various statistical measures to assess surface properties in the image.
The colors used on the display are gray shading for single bands, and RGB for multi-band composites. We can also perform image merge and sharpening to combine the advantages of both panchromatic (higher spatial resolution) and color imagery (better differentiation of surface materials).
Keys for image analysis
Hyperspectral imagery
Spectral reflectance library--different materials reflect radiation differently
To meet the various information requirements in forest management, different data sources like field survey, aerial photography, and satellite imagery is used, depending on the level of detail required and the extension of the area under study.
Remote Sensing Data Acquisition,Scanning/Imaging systemsdaniyal rustam
full of concepts about RS data acquisition scanning and imaging systems. Best for students of remote sensing. in this presentation we briefly explained the concept of scanning in remote sensing.
hyperspectral remote sensing and its geological applicationsabhijeet_banerjee
this is an introductory presentation on hyperspectral remote sensing, which essential deals with the distinguishing features, imaging spectrometers and its types, and some of the geological applications of hyperspectral remote sensing.
This document help you to prepare Triangulation Network (TIN), Hillshade Map, Slope map, interpolation and Digital Elevation Model (DEM) in a area and how to interpret them.
A remote sensing system uses a detector to sense the reflected or emitted energy from the earth's surface, perhaps modified by the intervening atmosphere. The sensor can be on a satellite, aircraft, or drone. The sensor turns the energy into a voltage, which an analog to digital converter turns into a single integer value (called the Digital Number, or DN) for the energy. Alternatively a digital detector can store the DN directly. We can then display this value with an appropriate color to build up an image of the region sensed by the system. The DN represents the energy sensed by the sensor in a particular part of the electromagnetic spectrum, emitted or reflected from a particular region. The principles can also be applied to sonar imagery, especially useful in water where sound penetrates readily whereas electromagnetic energy attenuates rapidly.
Definitions,
Remote sensing systems can be active or passive: active systems put out their own source of energy (a large "flash bulb") whereas passive systems use solar energy reflected from the surface or thermal energy emitted by the surface. Active systems can achieve higher resolution.
Satellite resolution considers four things: spatial, spectral, radiometric, and temporal resolution.
Electromagnetic radiation and the atmosphere control many aspects of a remote sensing system.
Satellite orbits determine many characteristics of the imagery, what the satellite sees, and how often it revisits an area.
The signal to noise ratio is important for the design of remote sensing systems.
Satellite band tradeoffs.
Interpreting satellite reflectance patterns and images uses various statistical measures to assess surface properties in the image.
The colors used on the display are gray shading for single bands, and RGB for multi-band composites. We can also perform image merge and sharpening to combine the advantages of both panchromatic (higher spatial resolution) and color imagery (better differentiation of surface materials).
Keys for image analysis
Hyperspectral imagery
Spectral reflectance library--different materials reflect radiation differently
Presentation at workshop: Reducing the costs of GHG estimates in agriculture to inform low emissions development
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Sponsored by the CGIAR Research Program on Climate Change, Agriculture and Food Security (CCAFS) and the Food and Agriculture Organization of the United Nations (FAO)
CAN CROP MANAGEMENT IMPROVE EMISSIONS SAVINGS?: PRELIMINARY RESULTS OF THE OP...Bioenergy Crops
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Forest Biomass Estimation using GIS.pptx
1. Forest Biomass Estimation using GIS
A Group Presentation on
GIS Application in Natural Resources FSE (701)
Group: Syntax
S.N. Name Class Roll no. S.N. Name Class Roll no.
1. Binita K.C. 5 5. Rabin Thapa 25
2. Kusum Saru 15 6. Santosh Ghimire 34
3. Niranjan Paudel 19 7. Susmita Khanal 39
4. Prabesh Adhikari 22 8. Yamuna Paudel 43
Submitted to: Assistant Professor Jeetendra Gautam
2. OUTLINE OF THE PRESENTATION
INTRODUCTION
OBJECTIVES
METHODOLOGY
FINDINGS AND RESULT
CONCLUSION
REFERENCES
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3. INTRODUCTION
Biomass is defined as mass of live or dead organic matter that includes the above-
ground and below-ground living biomass, dead mass, and litter (GTOS, 2009).
The largest carbon pool are typically stored in the above-ground living biomass. Thus
estimating above-ground forest biomass (AGB) is the most important step in
quantifying carbon stocks from forests (Gibbs et al., 2007).
The most accurate ways of calculating biomass data is based on field measurement
through destructive sampling or allometric equations method (Englhart et al., 2011).
However, these methods are often cost and time consuming, labor intensive, have
limited spatial distribution, and impractical especially in remote areas (Englhart et al.,
2011).
Remote sensing techniques have the capacity to overcome the limitations of
conventional field measurement methods and have now become the primary source in
estimating AGB (Lu, 2006).
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4. INTRODUCTION
These methods have been explored in terms of biomass and its changes to increase our
understanding of the role of forests in the carbon cycle for greenhouse gas inventories
and terrestrial carbon accounting (Muukkonen & Heiskanen, 2007).
Although much research has explored biomass estimation using remote sensing
technology methods to select suitable variables from remote sensing data and develop
estimation models suitable for specific studies are still poorly understood.
It is crucial to summarize the current status of remote sensing-based biomass
estimation techniques and discuss potential solutions to improve biomass estimation
performance.
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5. OBJECTIVES
General Objective:
To estimate the biomass of forest using GIS.
Specific Objective:
To calculate above ground biomass of Milanchowk CF from field inventory.
To establish a regression model between aboveground biomass and Sentinel 2
image.
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6. METHODOLOGY
Study Area:
The study was carried out in the
Milanchowk Community Forest, located
in Chitlang, Makawapur District.
It is extended from 27.34'52" N to
27.40'59"N and 85.01'21"E to 85.12'20"E
The average annual rainfall has been
recorded as 1863mm/year.
The dominant species of the study area
are Pinus and Quercus species.
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7. METHODOLOGY
Methodology Steps:
1) Download Sentinel 2 imaginary from USGS Earth Explorer.
2) Add Sentinel 2 imaginary data in Arc GIS 10.8 and calculate NDVI value.
3) Add boundary and sample plot point of CF.
4) Calculate Red band, Green bend, Blue band, NIR and NDVI value of
sample point.
5) Develop equation (Biomass vs Red, Green, Blue, NIR, NDVI Value) from
R-Studio programming software.
6) Validation Analysis using Paired t-test.
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8. METHODOLOGY
Data Collection:
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S.N. Data collection Activities
1. Primary data
collection
The systematic sampling method with 10m * 10m sample plot
is used for field measurement.
The biomass is estimated by using the equation: AGB =
0.0509 * pD2H (Where, AGB = above-ground tree biomass
[kg]; p = wood specific gravity [g/cm3; D = tree diameter at
breast height [cm]; and H = tree height [m])
Sentinel 2 image is used to calculated NDVI Value.
2. Secondary data
collection
Books
Journals
Article
Reports
9. FINDINGS AND RESULT
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Sample plot Biomass (kg)
1 1602
2 1429
3 1490
4 948
5 2164
6 1956
7 1253
8 572
9 1479
10 1080
11 1094
12 653
13 723
14 1814
15 1118
16 1113
17 845
18 422
19 1669
20 1847
Out of 30 sample plots, biomass estimation is done
from 20 sample plots which are used to generate the
biomass equation.
The maximum, minimum and average biomass
estimates from 20 sample plot of Milanchowk C.F.
are 2164 kg, 422 kg and 1263 kg respectively.
Biomass estimation
10. FINDINGS AND RESULT
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NDVI Value:
The high, low and average
NDVI value of Milanchowk
C.F. are 0.38033, 0.23325 and
0.322 respectively.
12. FINDINGS AND RESULT
Equation formulation:
To develop the biomass equation, five independent variables are used i.e.
(Biomass ~ Red band, Green band, Blue band, NIR, NDVI value).
Linear regression equation is used to fit dependent variable with independent
variables.
The fit regression equation derived from biomass modelling is:
Biomass ~ A + B * Red + C * Green + D * Blue + E * NIR + G * NDVI
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13. FINDINGS AND RESULT
The resultant data obtained from R- programme are:
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Constant Value
A -7.153034e+03
B -5.855211e+01
C -8.727644e+00
D 4.992052e+01
E 2.665179e+01
G -1.767242e+05
14. FINDINGS AND RESULT
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Equation Validation Analysis:
Ten sample plots are used for equation
validation analysis.
The resultant p value obtained from paired t–
test is p=0.08756 > 0.05, which indicates
above biomass equation is valid.
15. CONCLUSION
The maximum, minimum and average biomass are estimated as 2164 kg, 422 kg and
1263 kg respectively.
The high, low and average NDVI value are 0.38033, 0.23325 and 0.322 respectively.
The best fitted regression equation derived from biomass modelling is Biomass ~ A +
B * Red + C * Green + D * Blue + E * NIR + G * NDVI .
The biomass equation developed from this study can be used by the relevant
institutions, organizations and academics for research purposes as well as forest
management authorities.
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16. REFERENCES
Englhart, S., Keuck, V. & Siegert, F. (2011). Aboveground biomass retrieval in tropical
forest. Remote Sensing of Environment 115, pp. 1260-1271.
Gibbs, H.K., Brown, S., Niles, J.O. & Foley, J.A. (2007). Monitoring and estimating
tropical forest carbon stocks: making REDD a reality. Environmental Research Letters 2
(4), 13pp.
GTOS (Global Terrestrial Observing System). (2009). Assessment of the status of the
development of the standards for the terrestrial essential climate variables: Biomass.
Report FAO.
Lu, D.S. (2006). The potential and challenge of remote sensing-based biomass
estimation. International Journal of Remote Sensing, 27 (7), pp. 1297-1328.
Muukkonen, P. & Heiskanen, J. (2007). Biomass estimation over a large area based on
standwise forest inventory data and ASTER and MODIS satellite data: A possibility to
verify carbon inventories. Remote Sensing of Environment, 107(4), 617-624.
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