Mapping from space: Remote Sensing for migratory shorebird … · 2020-07-14 · Bahía Lomas...
Transcript of Mapping from space: Remote Sensing for migratory shorebird … · 2020-07-14 · Bahía Lomas...
Mapping from space: Remote Sensing for migratory shorebird conservation
at Bahia Lomas Ramsar Site
Dr. Paula Lightfoot
Dr. Fabio A. Labra
Webinar structure
• Introduction
• Using Sentinel-2 to Map Intertidal Extent at Bahía
Lomas Ramsar Site
• Using Remote Sensing Imagery to Model Migrant Bird
Habitat at Bahía Lomas Ramsar Site
• Questions and answers
Background
• This webinar presents the results of the pilot project
• "USING EARTH OBSERVATION TO DETERMINE DISTRIBUTION OF SUITABLE
HABITAT FOR MIGRATORY SHOREBIRDS: CASE STUDY OF BAHÍA LOMAS
RAMSAR SITE“
• This project was funded by the Department for the Environment, Food & Rural
Affairs of the United Kingdom government
• This is the first project managed and executed under the Southern Observation
Alliance of the Earth (Austral Earth Observation Alliance, AEOA).
Austral Earth Observation Alliance
• The Austral Earth Observation Alliance is a virtual centre of excellence to bring
together providers and users of EO enabling them to work together on common
problems to exploit EO in the South Atlantic and South American region
• Joint Nature Conservation Committee
• South Atlantic Environmental Research Institute
• Universidad de Magallanes
• Universidad Santo Tomás
• Universidad de Chile
• University of Dundee
Using Sentinel-2 to Map Intertidal Extent at Bahía Lomas Ramsar Site
Dr Paula Lightfoot, Earth Observation Specialist
Dr Gwawr Jones, Senior Earth Observation Specialist
July 15th, 2020
Introduction
Bahía Lomas Ramsar site is a 150km2 tidal flat in Tierra del Fuego, southern Chile.
It is a key wintering site for many wading birds, including Red Knot, Calidris canutus.
Red Knot have suffered a severe global population decline, possibly due to poor food
supply at their wintering sites.
Information on the distribution of key
habitats and prey species is essential
to inform conservation management.
Red Knots in flight over Bahía Lomas © Antonio LarreaRed Knot © G. Breese
Intertidal Extent Mapping
A map of the extent of the intertidal area at Bahía Lomas was needed to:
• help predict the distribution of shorebird habitat and prey species
• monitor change e.g. due to seismic movement or sea level rise
• validate the shoreward boundary of the Ramsar site.
This project investigated using Sentinel-2 imagery to map intertidal extent at Bahía Lomas.
Sentinel-2Sentinel-2 is a mission from Copernicus,
the Earth Observation programme run by
the European Commission and European
Space Agency.
Twin satellites, Sentinel-2A and Sentinel-2B
collect multispectral imagery, acquiring new data
every few days since 2015.
JNCC process Sentinel-2 imagery to create ‘analysis-
ready data’, a surface reflectance raster containing 10
bands at 10 metres resolution.
Sentinel-2 analysis-ready data has many applications,
including habitat mapping, condition monitoring and
change detection.
Sentinel-2
• Sentinel-2 imagery is supplied as a grid of tiles with unique alphanumeric codes.
Each tile measures 100km x 100km.
• Bahía Lomas Ramsar site is covered by tiles 19FDB and 19FEB and relative
orbits 67 and 110.
• Image acquisition time at Bahía Lomas is around 14:00 UCT (11:00 local time).
Coast X-Ray
Coast X-Ray is an approach for mapping intertidal extent in near real-time by
measuring water occurrence frequency using Sentinel-2.
It was developed by Scottish Government’s Dynamic Coast project to meet national
requirements for monitoring and coastal management.
The Dynamic Coast team kindly supported JNCC by trialling the Coast X-Ray
approach with Sentinel-2 data for Bahía Lomas.
http://www.dynamiccoast.com/
Coast X-Ray Method• Create a grid of 90 km2 hexagons covering the
coastal area.
• In each grid cell, create a ‘stack’ of cloud-free
Sentinel-2 images for a date range (September
2015 – January 2020).
• Generate Normalised Difference Water Index
(NDWI) each Sentinel-2 image in the stack.
• Classify pixels with NDWI > 0.2 as ‘water’.
• For each pixel in the image stack, calculate the % of
total images in which it is classified as ‘water’.
• The final output is a raster file in which each pixel
has a water occurrence value of 0 – 100.
𝐍𝐃𝐖𝐈 =𝐆𝐫𝐞𝐞𝐧 − 𝐍𝐞𝐚𝐫 𝐈𝐧𝐟𝐫𝐚𝐫𝐞𝐝
𝐆𝐫𝐞𝐞𝐧 + 𝐍𝐞𝐚𝐫 𝐈𝐧𝐟𝐫𝐚𝐫𝐞𝐝
Developed in Google Earth Engine
Coast X-Ray Water Occurrence RasterUsers can view the results and the input data on an interactive map here:
https://jamesmfitton.users.earthengine.app/view/coastxray
Coast X-Ray Water Occurrence Raster
The water occurrence
raster produced by the
Coast X-Ray method has
been provided to the
Universidad Santo Tomás
as an output of this
project.
• A map of the intertidal
extent can be created by
reclassifying the water
occurrence raster values.
• In theory, water occurrence
values should be
reclassified as:
0 = land
1-99 = intertidal zone
100 = sea
• However, this misclassifies
large areas of both sea and
land as intertidal.
Intertidal Extent Map
• A water occurrence
value of 5 appears best
for defining the high tide
limit.
• A value of 97.5 appears
best for defining the low
tide limit.
• Both values cause
some misclassification
which requires manual
editing.
Intertidal Extent Map
Two intertidal extent vector files derived from the Coast X-Ray water occurrence raster
have been provided to Universidad Santo Tomás as outputs of this project.
Intertidal Extent Map
Map 1. Clipped to a 12 km buffer around the Bahía
Lomas Ramsar site boundary, but not edited.
Map 2: Clipped to a 12 km buffer around the Bahía
Lomas Ramsar site boundary and manually edited
to remove misclassifications.
NDWI generated from Sentinel-2 imagery acquired on
a low spring tide on 12th May 2019
Normalised Difference Water Index
• In this example, there is good separation of NDWI value ranges for ‘sea’ and ‘intertidal’.
• ‘Land’ samples have lower NDWI values than ‘intertidal’, but there is overlap between the value ranges.
• The range of ‘intertidal’ NDWI values exceeds 0.2 (the threshold for water in the Coast X-Ray method)
• Turbid areas of sea have low NDWI values, which can lead to misclassification of water as land.
• Topographic shadows have high NDWI values, which can lead to misclassification of land as water.
NDWI values of randomly generated sample points
(n = 500 per class)
• As expected, ‘intertidal’ and ‘sea’ have similar NDWI value ranges when the intertidal zone is immersed.
• Low outlier values for ‘sea’ are the result of unmasked cloud.
• High outlier values for ‘land’ are the result of topographic shadow misclassified as water. The effect is
greater in this imagery from July than in the May imagery on the previous slide.
• Despite overlapping NDWI value ranges for ‘land’ and ‘intertidal’, there is a clear high water boundary.
Normalised Difference Water IndexNDWI generated from Sentinel-2 imagery acquired on
a high spring tide on 14th July 2018
NDWI values of randomly generated sample points
(n = 500 per class)
Future Research Opportunities• Explore the use of other indices in combination with NDWI to classify ‘water’ and ‘land’.
• Normalised Difference Vegetation Index (NDVI) could help to delineate the shoreward boundary and reduce
misclassification due to topographic shadow.
• Modified Normalised Difference Water Index (mNDWI) could reduce misclassification caused by turbidity.
• JNCC have produced analysis-ready Sentinel-2 data for 33 dates from 2016 to 2020, providing cloud-free
imagery of high and low spring tides. This will aid future research.
Future Research Opportunities
• The stack of Sentinel-2 images used to generate the Coast X-Ray water occurrence map may
not represent the full tidal range.
• Obtain locally referenced tidal data for Punta Arenas to cross-reference with the dates of the
imagery used.
• Ideally the image stack should include examples of the highest and lowest tides, but this may
not be the case due to cloud cover and satellite acquisition time.
http://www.ioc-sealevelmonitoring.org/station.php?code=ptar2
Future Research Opportunities
• Investigate potential of using Sentinel-1 radar data for mapping water occurrence
• This could improve the likelihood of obtaining usable imagery for the full tidal range
➢ radar data is not affected by cloud.
➢ Sentinel-1 acquisition times are around 09:00 and 23:45 UCT (06:00 and 20:45 local time)
• Research is needed into the consistency of radar backscatter values for land and water using
imagery from different dates.
• JNCC have produced analysis-ready Sentinel-1 data for 27 dates from March to November
2019, providing imagery of high and low spring tides.
Acknowledgements
• The Dynamic Coast Team, particularly
James Fitton and Alistair Rennie, for the
Coast X-Ray outputs.
• UK Government Department for
Environment, Food & Rural Affairs for
funding this collaborative project.
• Universidad Santo Tomás and Joint
Nature Conservation Committee as the
main partners in this project.
• Austral Earth Observation Alliance for
enabling this project by fostering
collaboration opportunities.
Mapping from space: Remote Sensing for migratory shorebird conservation
at Bahia Lomas Ramsar Site
Dr Fabio A. Labra
15th July 2020
Introduction
• Conservation and management efforts often require spatially explicit description of
habitats and species distribution as an input for research or decision process
• In addition to Calidris canutus, Bahia Lomas harbours other important
conservation targets
© Antonio Larrea
Introduction
• Conservation and management efforts often require spatially explicit description of
habitats and species distribution as an input for research or decision process
• In addition to Calidris canutus, Bahia Lomas harbours other important
conservation targets
• Accurate habitat maps are needed to inform conservation management
© Antonio Larrea
Earth Observation can assist conservation
• Remote sensing data such as satellite imagery can help us to obtain accurate distribution maps, by using statistical models to infer the distribution of species from those images together with geo-located points where species have been observed
Darina solenoidesDarina solenoides
Workflow
SDMMaxEnt
Satellite image
Intertidal habitat extent
Species presence
Clip, RTOA
Gathering spatial information
Processing Modelling Mapping
Workflow: Darina solenoides
SDMMaxEnt
Clip, RTOA
Gathering spatial information
Processing Modelling Mapping
Satellite Images
• Landsat 8
• Sentinel 2
• WorldView-2
BandsRed, Green, Blue, Near Infrared
BandsRed, Green, Blue, Near Infrared
BandsRed, Green, Blue, Near Infrared
Landsat 8 (30m)
February 6, 2020 August 25, 2019
Sentinel 2 (10m)
February 8, 2020 August 25, 2019
WorldView-2 (0.5 m)2013-2016
Model fit:• We observed very good model
fit to observed presence data sets across all three EO imagery scenes
• In both Polychaete worms and Sarcocornia magellanica, a scale effect is apparent
• This may reflect the imbalance in the presence sample size with the resolution and number of image pixels
a)
b)
c)
Darina solenoides
Polychaete worms
Sarcocornia magellanica
L8, 6 febrero 2020 L8, 25 agosto 2019
S2, 8 febrero 2020 S2, 25 agosto 2019
L8, 6 febrero 2020 L8, 25 agosto 2019
S2, 8 febrero 2020 S2, 25 agosto 2019
L8, 6 febrero 2020 L8, 25 agosto 2019
S2, 8 febrero 2020 S2, 25 agosto 2019
Darina solenoides Polychaetes
Sarcocornia magellanica True color image
Distribution area:
• We estimated the covered pixel area for each of these conservation targets, and examined the possible effects of Sensor image scale of resolution
• Intertidal invertebrates exhibit a strong effect of scale, while there´s no significant effect for Sarcocornia magellanica
Results
• It is possible to characterize the distribution of habitats for migratory birds by using earth observation images
• Darina solenoides shows a wide distribution in the Bahía Lomas Nature Sanctuary, covering between 35% and 40% of the surface area of the Nature Sanctuary.
• In the case of polychaete worms, they cover between 43% and 48% of the Sanctuary surface, while Sarcocornia magellanicahas a more restricted distribution, which covers between 12% and 13% of the Sanctuary surface.
Future Research Opportunities
• Investigate the distribution pattern at a species level for the most
abundant polychaete taxa
• Estimate Darina solenoids and polychaete biomass or standing stock by
building onto the distribution modelling work. This may be achieved by
further field sampling, including the empirical estimation of biomass.
• Further development of sampling and modelling to assess temporal and
spatial variability in Sarcocornia magellanica distribution and phenology
across the Nature Sanctuary.
• Incorporate other modelling approaches, including machine learning
algorithms such as Boosted Regression Trees, Random Forest or
Support Vector Machines, and contrasting their performance with other
methods such as GLM, GAM. Lm GLM GAM RF
Future Research Opportunities
• Exploring the opportunities to apply these methods in other migratory bird habitats, by adding
sampling and image analysis to the tools available for conservation effors focused on migrant
shorebird species
Darina solenoides Sarcocornia magellanicaPolychaetes
Acknowledgements
• The Centro Bahia Lomas Team, particularly
Carmen Espoz and Gabriela Garrido.
• UK Government Department for
Environment, Food & Rural Affairs for
funding this collaborative project.
• Field sampling has been funded over the
years by several institutions including MMA,
ENAP, UST and Manomet.
• Sampling was made possible by the
collaboration and help in the fieldwork and lab
by Ricardo Matus, Alejandra Ponce, Olivia
Blank, Gabriela González, Antonio Larrea,
Melissa Villagrán, among many others