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2 changes: 1 addition & 1 deletion _quarto.yml
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type: book

book:
title: "Assesing uncertanties related to satellite remote sensing indices to estimate Gross Primary Production"
title: "Assesing uncertanties related to the use of satellite remote sensing indices to estimate Gross Primary Production"
subtitle: "By"
author:
- name: "Ronny A. Hernández Mora"
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19 changes: 10 additions & 9 deletions abstract.qmd
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Methods to quantify Gross Primary Production (GPP) are classified into two
categories: Eddy Covariance techniques (EC) and satellite data-driven. EC
techniques can measure carbon fluxes directly, albeit of spatial constraints.
techniques can measure carbon fluxes directly, albeit with spatial constraints.
Satellite data-driven methods are promising because they overcome spatial
constraints associated with EC techniques. However, there are challenges
associated with an increase in uncertainty when estimating GPP from
satellite-driven products such as mixed pixels, cloud cover, and the ability of
the sensor to retrieve vegetation under saturation conditions in high biomass
environments. Therefore an effort to analyze and quantify the uncertainty of GPP
products derived from satellite platforms is needed. Here we present how
commonly used satellite vegetation indices (NDVI, EVI, CCI, and NIRv) can impact
the uncertainty in the GPP estimation compared with direct methods such as EC
constraints associated with EC techniques. However, satellite-driven products
have potentially greater uncertainty than EC methods for GPP estimation such as
mixed pixels, cloud cover, and the ability of the sensor to retrieve vegetation
under saturation conditions in high biomass environments. Therefore, an effort
to analyze and quantify the uncertainty of GPP products derived from satellite
platforms is needed. This study quatifies the uncertainty of commonly used
satellite vegetation indices such as Normalized Difference Vegetation Index (NDVI), Enhance
Vegetation Index (EVI), Chlorophyll/Carotenoid Index (CCI), and Near-Infrared Reflectance Index (NIRv)
for GPP estimation compared with direct methods such as EC
measurements. We conduct this study on three different sites: University of
Michigan Biological Station (USA), the Borden Forest Research Station flux-site
(Canada) and Bartlett Experimental Forest (USA) using traditional regression
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161 changes: 78 additions & 83 deletions chapter_1_intro.qmd
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The study and assessment of ecosystem dynamics have greatly benefited from the
development and advances of the remote sensing field [@running_continuous_2004; @baldocchi_how_2020-1]
coupled with the growing freely available remote sensing
resources [@montero_standardized_2023]. Elements in the Earth surface exhibit
data [@xiao_remote_2019]. Elements on the Earth surface exhibit
distinctive spectral signatures arising from their physical properties and
interactions with electromagnetic radiation. Environmental factors can affect
these interactions modifying the spectral signatures which can provide insights
about surface process when measured by remote
sensing instruments [@montero_standardized_2023].
interactions with electromagnetic radiation [@montero_standardized_2023].
Environmental factors (fires, floods, drought, etc) can affect these
interactions modifying the spectral signatures which can provide insights about
surface process when measured by remote sensing instruments [@montero_standardized_2023].

The launch in the 1970's of the Earth Resources Technology Satellite (ERTS),
later known as Landsat-1 [@houborg_advances_2015], initiated a new era in the
later known as Landsat-1 [@donato_landsat_nodate], initiated a new era in the
remote sensing field of the terrestrial biosphere, with a special focus on
vegetation monitoring [@montero_standardized_2023]. With information available
about spectral bands, studies about their relations to biophysical
characteristics became an object of study to estimate biomass and photosynthetic
activity [@myneni_estimation_1997]

In fact, one application of remote sensing have been the development of
vegetation indices to study the characteristics of vegetation canopies and
functioning [@houborg_advances_2015] Vegetation indices can give us information
about the status of the vegetation given the information derived from mathematical
equations from the values of two or more spectral bands, typically derived from
satellite images. [@zeng_optical_2022]. Their interpretation is based on the
theoretical background about the interaction of the light with vegetation
[@zeng_optical_2022]
vegetation indices (VI) to study the characteristics of vegetation canopies and
functioning [@houborg_advances_2015]. VIs are a function of two or more
spectral bands, typically derived from satellite images [@zeng_optical_2022].
that can contain information about the status of the vegetation, biochemical
characteristics, structural characteristics such as Leaf Area Index
(LAI), among others [@huete_overview_2002].

Early studies about spectral bands relations, lead to the development of the
NDVI which showed how the NIR and Red ratio had advantages over other bands
ratios for monitoring vegetation [@tucker1979red]. It rationale lays in the
interplay of the chlorophyll absorbing red spectral region with the
non-absorbing leaf reflectance signal in the NIR region, that can give optical
measurements of the vegetation greenness and other biophysical processes.
[@ramachandran_modis_2010]

One of the advantages of NDVI is that the ratio normalize values with large
variances [@ramachandran_modis_2010]. Nonetheless, this
VI have disadvantages such as sensitivy to soil background and saturation at
high biomass [@huete_overview_2002]. To overcome
this problem, the EVI was designed to improve vegetation characterizations such
NDVI, which showed how the NIR and Red ratio had advantages over other bands
ratios for monitoring vegetation biomass and structure given surface reflectance
measurements in the shortwave spectrum [@tucker1979red; @richardson1977distinguishing].
The basis of NDVI rests in the fact that chlorophyll absorption leads to a
decrease in red reflectance with increasing green vegetation relative to the
NIR reflectance, that is minimally impacted by chlrophyll absorption [@ramachandran_modis_2010].

The use of a relative indicator serves to reduce the effect of factors such as
canopy spatial structure and non-photosynthetic vegetation on relationships
between NDVI and biophysical variables such as biomass or absorbed
photosynthetically active radiation variances [@sellers_canopy_1987; @ramachandran_modis_2010].
Nonetheless, NDVI is sensitive to soil background and saturation at
high biomass [@huete_overview_2002]. To overcome this problem, the Enhance
Vegetation Index (EVI) was designed to improve vegetation characterizations such
as canopy greenness without soil background sensitivity and aerosol variations
by combining the blue, red, and NIR bands [@huete1988soil]. EVI is also less
prone to saturate at high biomass instances [@gao_opticalbiophysical_2000]

The ability to combine spectral regions, coupled with advancements and the
The ability to combine reflectance from multiple spectral bands, coupled with advancements and the
development of new sensor technologies introducing additional bands or different
spectral characteristics, has created opportunities to develop multiple VIs and
the total number of indices have grown steadily [@zeng_optical_2022]. These
Expand All @@ -54,48 +55,55 @@ enhance existing estimations across different ecosystems [@ramachandran_modis_20
According to the Awesome Spectral Indices open community catalogue (version
4.0.0), there are 127 spectral indices designed to monitor vegetation. The aim
behind the ongoing development of new VIs is to achieve a more accurate mapping
of ecosystem processes **such as GPP**. [@montero_standardized_2023]. These
of ecosystem variables such as GPP. [@montero_standardized_2023]. These
indices can be classified into 3 main categories: biophysical, biochemical and
physiological properties [@zeng_optical_2022] **Describe the categories**

One important metric to understand ecosystems processes is GPP. At the time, VIs
One important variable to understand ecosystems processes is GPP. At present, VIs
derived from satellites cannot directly estimate GPP [@gensheimer_convolutional_2022]
and instead, instruments like eddy covariance have been the traditional method
to estimate GPP more directly [@baldocchi_how_2020-1].

GPP represents the overall quantity of leaf photosynthesis, playing a crucial
role in the carbon cycle [@xiao_remote_2019]. GPP is responsive to a range
of factors, including abiotic elements such as radiation, temperature, and
precipitation [@beer_terrestrial_2010], as well as biotic factors like
GPP represents the total amount of carbon compunds produced by plant photosynthesis
in a given period of time [@ashton_managing_2012]. GPP plays a crucial
role in the carbon cycle since it quantifies the ability of vegetation to fix
carbon from the atmosphere using only solar energy and nutrients [@xiao_remote_2019].
GPP is responsive to a range of factors, including abiotic elements such as
radiation, temperature, and precipitation [@beer_terrestrial_2010], as well as biotic factors like
vegetation type, leaf chemical traits, and species composition [@musavi_stand_2017].

Some of the carbon taken in by GPP is release back to the atmosphere through
plant respiration (autotrophic respiration), and the difference between GPP and
plant respiration is called Net Primary Productivity (NPP) [@lieth1975modeling; @xiao_remote_2019].
GPP, along with Ecosystem Respiration (ER), which includes both autotrophic and
heterotrophic respiration, together determines Net Ecosystem Exchange (NEE)
[@xiao_remote_2019].

EC is a method used to measure the exchange of energy and materials between
ecosystems and the atmosphere within an area that can range from a few hundred
meters to a few kilometers [@pabon-moreno_potential_2022]. Specifically, EC
systems measure NEE, which has to be break down into its parts: GPP and
respiration **for quantifycation** [@reichstein_separation_2005]. Despite being
a more directly method to estimate GPP, EC systems have a spatial constrain that
depends on the tower flux footprint [@baldocchi_how_2020-1].
[@xiao_remote_2019]. NEE is fundamental to the planetary carbon cycle as it
represents the net accumulation or loss of carbon by the ecosystem. Measurement
of GPP and NEE are critical to understanding the role of the biosphere in the
carbon cycle as well as the status and trends of vegetation productivity [@schimel_terrestrial_1995]

Eddy Covariance (EC) is a method used to measure the exchange of energy and
materials between ecosystems and the atmosphere within an area that can range
from a few hundred meters to a few kilometers [@pabon-moreno_potential_2022].
Specifically, EC methods can estimate GPP in-situ at temporal resolution of
seconds, by subtracting estimates of respiration from chamber measurements or models
from direct measurements of NEE [@reichstein_separation_2005]. However, EC
estimates are both, costly and limited in spatial coverage [@baldocchi_how_2020-1].
Also, uncertainties from this method lies in the typical increase in spatial and temporal
variability in GPP over heteregeneous landscapes such as forest boundaries [@reinmann_edge_2017].
The prevalent practice of taking measurements primarily from intact forests
introduces the risk of potentially misleading estimations for the broader forest
being quantified, given the potential differences in dynamics between edge and
interior environments [@smith_piecing_2018].

Since direct GPP measurements from satellites are not presently available, one
of the primary objectives of remote sensing is to enhance GPP estimation
accuracy without the spatial constriction [@xiao_remote_2019]. In this context,
EC values prove invaluable as a comparative metric when contrasting VIs values
of the primary objectives of remote sensing is to enhance the spatial coverage
of EC GPP estimates [@xiao_remote_2019]. In this context,
EC values prove invaluable as information for calibrating VIs values
with GPP inferred from flux towers [@ramachandran_modis_2010]. The utilization
of EC measurements bridges the gap in GPP assessment, providing a practical
means to evaluate and refine the reliability of remotely sensed data against
ground-based observations [@xiao_remote_2019]. This methodological approach
aligns with the overarching goal of leveraging remote sensing techniques to
advance our understanding of the magnitude, spatial patterns, inter annual
variability and long-term trends of ecosystem Carbon dynamics at landscape,
regional and global scales [@xiao_remote_2019].
ground-based observations [@xiao_remote_2019].

Various methods exist for estimating GPP through satellite measurements.
Satellite-derived VIs serve as commonly employed proxies for GPP, whereas
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However, both Light Use Efficiency (LUE) models and process-based models demand
a multitude of inputs, some of which may not be readily available for all sites.
In such cases, a data-driven approach becomes particularly advantageous, and VIs
serve as effective proxies for GPP estimation. Notably, emerging VIs like NIRv
demonstrate a capability to account for 68% of the monthly variability in GPP
across fluxnet sites [@badgley_terrestrial_2019]. Additionally, indices like
CCI, a pigment-based index designed to capture carotenoid/chlorophyll ratios
serve as effective proxies for GPP estimation. Notably, emerging VIs like
the Near-Infrared Reflectance Index (NIRv) demonstrate a capability to account
for 68% of the monthly variability in GPP across 105 fluxnet sites [@badgley_terrestrial_2019].
Additionally, indices like CCI, a pigment-based index designed to capture carotenoid/chlorophyll ratios
during seasonal photosynthetic activity in evergreen leaves [@gamon_remotely_2016],
have demonstrated proficiency as estimators of GPP in certain forest types. These
indices offer valuable insights into the dynamics of vegetation productivity.

Despite the notable progress in VIs development and their user-friendly
applications, their effective use demands a experience and a strong theoretical
background to navigate potential pitfalls and ensure accurate and meaningful
interpretations of the data [@zeng_optical_2022]. There is a consensus that no
single VI can be universally applied to address every problem or situation.
Thus, a meticulous understanding of the specific context and characteristics of
the site is essential to derive more accurate and insightful information from
the data [@zeng_optical_2022].

Uncertainty poses additional challenges to remote sensing applications, with
applications there is a consensus that no single VI can be universally applied
to address every GPP estimation across
species and time periods, even for a single biome [@zeng_optical_2022].
VI measurement error poses additional challenges to remote sensing applications, with
diverse sources affecting satellite-derived data, including atmospheric effects,
retrieval errors, cloud contamination, and sensor degradation
[@van_leeuwen_multi-sensor_2006; @fang_theoretical_2012]. Another contributing
factor to uncertainties lies in the variations of carbon uptake and storage,
which can be higher in forest edges. [@reinmann_edge_2017] The prevalent
practice of taking measurements primarily from intact forests introduces the
risk of potentially misleading estimations for the broader forest being
quantified, given the potential differences in dynamics between edge and
interior environments [@smith_piecing_2018].

Moreover, while emerging indices show promise as better proxies for
physiological processes, ongoing technological developments have limitations in
terms of spatial/temporal resolution which can still be not the best to conduct
more studies that can be applied easily to more ecosystems [@zeng_optical_2022].
One notable example is SIF, which holds the advantage of being directly related
to photosynthetic activity [@magney_mechanistic_2019]. In contrast, Vegetation
Indices (VIs) are primarily associated with photosynthetic capacity
[@sellers_canopy_1985]
[@van_leeuwen_multi-sensor_2006; @fang_theoretical_2012]. Thus, a quantitative
and rigorous understanding of the specific context and
characteristics of multiple sites is essential to understand the potential and
limits of VIs for GPP estimation over large extents of space and time. [@zeng_optical_2022].

Together with the advancement of new VIs, there has been a upsurge in data
analysis methods, specifically Machine Learning (ML) approaches, has garnered
Expand All @@ -171,10 +162,14 @@ sites play a pivotal role in influencing the accuracy and variability of
regional flux estimates derived from machine learning methods
[@papale_effect_2015].

In this study, I assess the advantages and contraints associated with the
utilization of 4 widely employed VIs for estimating GPP. The study specifically
focuses on VIs derived from the MODIS, which have long standing temporal records
and acceptable spatial resolution to study extended forest areas. The analysis
The goal of this study is to assess the advantages and contraints associated with the
utilization of 4 widely employed VIs for estimating GPP. The study is limited
to temperate broadleaf forests of Eastern United States of America and Canada
as it required consistent multi-annual EC GPP measurements over multiple sites
to quantify uncertainty related to spatial location of calibration data. The
VIs are derived from the Moderate Resolution Imaging Spectroradiometer (MODIS),
which have long standing temporal records and acceptable spatial resolution to
study extended forest areas. The analysis
employs both traditional regression methods and ML techniques to evaluate the
performance of these indices in estimating GPP. This methodological approach
seeks to provide a nuanced understanding of the efficacy and limitations of the
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## References

::: {#refs}
:::
:::
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