TDA/SAP Methodology Training Course Module 2 Section 5
USF - Satellite Observations in Support of LME Governance: A Case Study for Data Exchange in the Wider Caribbean LME
1. Frank Muller-Karger, Gerardo Toro-Farmer, Digna Rueda
Institute for Marine Remote Sensing
University of South Florida
Satellite Observations in Support of
LME Governance:
A Case Study for Data Exchange in the Wider
Caribbean LME
Exchange of Experiences on LME- related data and information
issues
Buenos Aires, Argentina, June, 2013
2. Requirement for Dynamic
LME Governance
2
Governance requires ‘knowledge’
(understanding of what is happening). Knowledge
has to be:
Co-derived (joint natural + social science effort)
Inexpensive to local governments
Timely
LMEs are ‘Large’: They require a synoptic
framework of observations
LME’s change continuously: They require time
series of observations
3. Synoptic ocean time series
3
Regional-global context to understand
processes, stocks, and diversity within
different parts of a dynamic LME
Means to quantitative measure change in
LME’s
Place point observations in regional
context
Initialize and validate simulations /
ecological forecasting
4. Today’s Tools
4
Atlas – today we can show dynamic aspects of
an ecosystem
Climatologies (monthly, annual) as ‘baseline’ to
measure
short-term change
Long-term trends
Occurrence and impacts of extreme events
Time series (observations and anomalies)
Other dynamic information: individual historic and
current observations, forecasts
5. Prototype datasets for the
Caribbean
5
Regional-scale and local satellite data
products
Printed Atlas: Wider Caribbean LME
Digital Atlas examples:
Caribbean Marine Atlas (IODE)
http://www.caribbeanmarineatlas.net/
NOAA Gulf of Mexico Data Atlas
http://gulfatlas.noaa.gov
6. Satellite derived synoptic
data
6
Sea surface temperature (SST) 1 km
Ocean color (turbidity, CHL, CDOM)250 m – 1
km
Wind 25 km
Sea Surface Height/currents ~100-
300 km
Sea Surface Salinity ~300
km
Geomorphological and Habitat: ~2 m
> 30 m
10. 10
Application 2: Satellite Time Series
Southern Caribbean upwelling system
20
21
22
23
24
25
26
27
28
29
30
20
21
22
23
24
25
26
27
28
29
30
-4
-3
-2
-1
0
1
2
3
4
Climatology
Time Series
Anomaly
Weekly time series (March 12-18, 2005)
20
21
22
23
24
25
26
27
28
29
30
°C
°C
Anomaly = Time series - Climatology
11. Application 2: Satellite Time Series
Southern Caribbean upwelling system (coastal SST anomalies time
series)
Longitude (°W)
9°
10°
11°
12°
9°
10°
11°
12°
-76° -74° -72° -70° -68° -66° -64° -62°
Latitude(°N) °CTime(year)
11
12. 12
Application 2: Satellite Time Series
Southern Caribbean upwelling system (coastal SST anomalies time
series)
°CTime(year)
Spanish sardine capture
crashed after two
consecutive years of weak
upwelling
14. 14
What is the relation between Climate
Change and Coral (benthic) health?
Eakin et al.
(2010)
Application 5: Thermal Stress and Coral Bleaching
A) Maximum NOAA Coral Reef Watch
Degree Heating Week (DHW) during
2005.
(B) means of coral bleached as either
percent live coral colonies (circles) or cover
(diamonds).
15. 15
Can we identify benthic composition?
Is Coral (benthic) coverage changing over
time?
• Benthic coverage is affected by natural /
anthropogenic events
• Need to monitor / understand interannual variations
and ecological shifts
Application 6: Mapping Benthic Coverage
Classified dataset based on Landsat for Looe Key Reef
(red: coral, brown: covered hardbottom, yellow: bare
hardbottom, green: sand. Palandro et al. (2008)
16. Decision Support Tools for an Ecosystem
Based Management
Developing a flexible framework for integrated,
distributed,
and interlinked regional coastal and marine data atlases
based on the NOAA Gulf of Mexico data atlas
16
Goals
Integrate scientific and socio-economic
information
through an online data atlas
to help visualize and analyze historical
datasets,
understand connectivity, trends, and
variability
17. Objectives:
• Identify and integrate additional specific data sets
• Implement a framework for embedding regional
data atlases
• Enhance the user interface of existing web-based
data atlas(es) for displaying, querying and
analyzing information, providing meaningful
statistics for decision-making
• Develop a prototype for a mobile platform
Decision Support Tools for Ecosystem-Based
Management
17
18. Decision Support Tools for Ecosystem-Based
Management
18
Gulf of Mexico Data Atlas
(NOAA)
http://gulfatlas.noaa.gov/
19. 19
Decision Support Tools for Ecosystem-Based
Management
Currents
(m s-1)
CHL long term annual climatology (mg m-3
)
Longitude
Latitude
-85 -80 -75 -70 -65 -60 -55 -50 -45
0
5
10
15
20
25
0.02
0.05
0.1
0.2
0.5
1
2
5
10
mask
Chlorophyll
(mg m-3)
Wind (m s-1)
Gulf of Mexico Data Atlas
(NOAA)
http://gulfatlas.noaa.gov/
20. 20
Use existing datasets developed for the
Caribbean LME atlas as initial layers for the IODE
Caribbean Marine Atlas:
(http://www.caribbeanmarineatlas.net/)
Link the Gulf of Mexico and Caribbean Atlases
Develop a framework for an integrated global
atlas that:
Uses existing (easily available) ocean and land
satellite data
Provides the framework and technology tools to
incorporate new regions around the world
Develop an inter-operable data platform
Recommendations
Editor's Notes
An important element of the knowledge base for LME governance are synoptic time series. For the ocean, satellite datasets provide relevant and timely information. They also provide
The SST climatology makes possible to characterize…
Higher SSTs during Sep-Oct
The SST climatology makes possible to characterize the upwelling cycle and its variability along the coast
Climatologies are baseline’ to measure short-term change, occurrence and impacts of extreme events
Anomalies (time series - climatology) allow a clear visualization of the real SST changes compared with the mean conditions.
In this example the warmest areas are the coastal upwelling, and second, the eastern Caribbean.
Clear visualization of the extension and duration of coastal SST anomalies
Sardine crash!
Clear visualization of the extension and duration of coastal SST anomalies
Sardine crash!
OJO: in grey No Significant values (p>0.05)
Warming most pronounced during the period with higher SSTs (Sep-Oct), which might imply more stress to certain organisms/ecosystems.
Upwelling getting warmer in the beginning of the upwelling season (Dec-Feb).
Tendency is calculated with anomalies
Relevant for fisheries … life cycles, spawning or reproduction months
High temperatures cause stress and mass bleaching events. Low temperatures also affect coral. Need to monitor temperature changes to understand ecological shifts.
Eakin CM, et al. (2010) Caribbean Corals in Crisis: Record Thermal Stress, Bleaching, and Mortality in 2005. PLoS ONE 5(11): e13969.
Palandro et al. (2008). Quantification of two decades of shallow-water coral reef habitat decline in the Florida Keys National Marine
Sanctuary using Landsat data ( 1984-2002 ). Remote Sensing of Environment, 112, 3388-3399