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Integrating Animal Borne Sensors (ABS) with SMARTS Climatology Model Improves Forecasts of Hurricane Intensity and Fishery Dynamics J.S. Ault, L.K. Shay, J. Luo, J. Brewster, N. Hammerschlag, P.C. Meyers, B. Jaimes and J.R. Rooker* University of Miami, Rosenstiel School of Marine and Atmospheric Science, Miami, FL 33149 USA *Texas A&M University, Galveston, Texas 77551 USA Abstract Hurricane intensity forecasting has been advanced by a new Systematically Merged Atlantic Regional Temperature and Salinity (SMARTS) climatology model that blends temperature and salinity fields from the World Ocean Atlas 2001 and Generalized Digital Environmental Model at 1/4° resolution. The two‐layer reduced gravity model framework facilitates robust daily estimates of isotherm depths from regional radar altimetry. In addition to tracking the depth of the 26 o C isotherm for hurricane intensity forecasting, several species of premier gamefish (e.g., Atlantic tarpon, blue marlin, tiger sharks) tagged with satellite‐telemetry devices equipped with temperature, depth, salinity and GPS sensors have demonstrated these species closely followed the seasonal progression of the 26 °C isotherm depth during their annual migrations throughout the Gulf of Mexico, southeastern Atlantic and Caribbean Sea. Tarpon sport‐fishing alone, for example, is a $6 billion industry in the United States; however, this valuable resource is vulnerable to exploitation and environmental changes. In this research we explored how an enhanced network of animal‐borne sensor deployments integrated within the SMARTS technology framework has the unique opportunity to improve hurricane forecasts and predictions of ocean fishery dynamics. Motivation and Background Minimum sea surface temperature threshold for hurricane formation: SST >26 o C (Palmen, 1948) Leipper (1972) introduced Ocean Heat Content: Integrated thermal energy from surface to 26 o C isotherm: Empirical approach to estimate OHC from satellite altimetry (Shay and Brewster, 2010). Ocean thermal structure is an important feedback mechanism (Chang and Anthes, 1978). Warm core eddies inhibit mixing and provide deep energy source for hurricanes (Shay et al., 2000; Jaimes and Shay, 2009). MLD D26 OHC SST 26°C dz T c OHC D z p ) 26 ( 26 ARGOS, XBT, AXBT, Moorings: 44,000 Profiles From 1998-2009 (Meyers et al., 2010) Tracking Fish Movements with Space-Age Technologies Ocean Heat Content Empirical Approach (Shay et al. , MWR, 2000) Reduced gravity (g’), H 20 , h (ocean mixed layer depth) GDEM. Blend and objectively map SHA from Jason-1, GFO, and Envisat (9.9, 17 and 35- d repeat track). Infer H 20 using mapped SHA and seasonal climatology. Estimate H 26 relative to H 20 (via ratio). Estimate OHC relative to 26 o C using H26, h, and SST. Upper ocean cooling induced by Hurricane Ivan (2004) over the Loop Current (LC) System Fish Locations Obtained from Satellite-Tag Deployments, 2001-2011 An example blue marlin (Makaira nigricans) movement track derived from satellite-based Popoff Archival Transmitting (PAT) tag deployed between July 3 rd to September 29 th 2004. Vertical temperature profile of the blue marlin during the 89 day deployment based on ARGOS transmitted PAT-tag data. The solid black line indicates the depth of 26 o C. White arrow indicates upwelling induced by Hurricane Ivan on September 15 th (see Fig. 5). Ocean Heat Content (OHC, see Fig. 1) derived from the blue marlin’s vertical temperature profile shown above. Summary SMARTS improves estimation of OHC in the North Atlantic Ocean basin when combined with satellite altimetry and SSTs (Meyers, 2011). In situ measurements are crucial to improve SMARTS. Combining high resolution ABS measurements with improved T,S tags in strong ocean fronts such as the Loop Current and its eddy field provides valuable observations for fisheries and SMARTS. A clear connection is emerging between the behaviors of fish and physical oceanographic processes (e.g., 26 o C isotherm depth, OHC). Need to take the next steps to quantitatively compare satellite-based fields with ABS in situ measurements. Assimilating the ABS measurements over the basin will provide key measurements for higher resolution ocean models that will improve coupled biological and physical models for assessing ecosystem stressors (i.e., hurricanes, oil spills, climate changes). We conclude that by extending the use of Animal Borne Sensors (ABS) data within the existing SMARTS technology framework can greatly improve understanding of the coupled dynamical behaviors of ocean‐atmosphere and fish stock migrations that may portend a new era of forecasting hurricane intensity and novel ecosystem‐based strategies for sustaining key ocean fisheries. Over the past decade, satellite-based tag technologies have facilitated an improved understanding of migrations, behavior patterns, and environmental preferences for a number of large marine fishes (such as tunas, billfish, sharks, and Atlantic tarpon) providing valuable information for resource managers to ensure protection and sustainability of these valuable and iconic fisheries. What Do Hurricanes and Tarpon Have in Common? They all prefer SST greater than 26 o C. Migration track and vertical temperature profile of Tarpon 116 Migration track and vertical temperature profile of Tarpon 86 Daily average temperatures (black dots) and associated monthly frequency distribution (histogram bars). Distribution of Sea Surface Height field on September 17 from altimetry; warm core eddy (WCE) and cold core eddy (CCE), , relative to the track of Hurricane Ivan. From Halliwell et al. (MWR 2011). Satellite-based SST before (left) and after (right) the passage of Ivan. SST from the HYbrid Coordinate Ocean Model (HYCOM). Bill. Boyce Don DeMaria Acknowledgments Research team from the Upper Ocean Dynamics Laboratory (LKS) gratefully acknowledges support from NOAA NESDIS (NA10OAR4320143) in the development and implementation of SMARTS for Global Ocean Heat Content Project; and NASA Hurricane Science Team (NNX09AC47G) and the NOAA Joint Hurricane Testbed (NA17RJ1226). Fish migration research appreciates the fiscal support from the Bonefish & Tarpon Trust, Robertson Foundation, Sanctuary Friends Foundation of the Florida Keys, Texas Parks & Wildlife Department, Tarpon Tomorrow, Texas Coastal Conservation Association, the Batchelor Foundation, West Coast Inland Navigation District, and Wells-Fargo. Upwelling Fig. 1 Fig. 2 Fig. 3 Fig. 4 Fig. 5 Fig. 6 Fig. 7 Atlantic tarpon (Megalops atlanticus) CCE WCE CCE Poster ID: B1173
Transcript
Page 1: Integrating Animal Borne Sensors (ABS) with SMARTS ...isotherm.rsmas.miami.edu/.../Ault_ASLO_Ocean_poster... · Satellite-Tag Deployments, 2001-2011 An example blue marlin (Makaira

Integrating Animal Borne Sensors (ABS) with SMARTS Climatology Model Improves Forecasts of Hurricane Intensity and Fishery Dynamics

J.S. Ault, L.K. Shay, J. Luo, J. Brewster, N. Hammerschlag, P.C. Meyers, B. Jaimes and J.R. Rooker* University of Miami, Rosenstiel School of Marine and Atmospheric Science, Miami, FL 33149 USA

*Texas A&M University, Galveston, Texas 77551 USA

Abstract Hurricane intensity forecasting has been advanced by a new Systematically Merged Atlantic Regional Temperature and Salinity (SMARTS) climatology model that blends temperature and salinity fields from the World Ocean Atlas 2001 and Generalized Digital Environmental Model at 1/4° resolution. The two‐layer reduced gravity model framework facilitates robust daily estimates of isotherm depths from regional radar altimetry. In addition to tracking the depth of the 26oC isotherm for hurricane intensity forecasting, several species of premier gamefish (e.g., Atlantic tarpon, blue marlin, tiger sharks) tagged with satellite‐telemetry devices equipped with temperature, depth, salinity and GPS sensors have demonstrated these species closely followed the seasonal progression of the 26 °C isotherm depth during their annual migrations throughout the Gulf of Mexico, southeastern Atlantic and Caribbean Sea. Tarpon sport‐fishing alone, for example, is a $6 billion industry in the United States; however, this valuable resource is vulnerable to exploitation and environmental changes. In this research we explored how an enhanced network of animal‐borne sensor deployments integrated within the SMARTS technology framework has the unique opportunity to improve hurricane forecasts and predictions of ocean fishery dynamics.

Motivation and Background

• Minimum sea surface temperature threshold for hurricane formation: SST >26oC (Palmen, 1948)

• Leipper (1972) introduced Ocean Heat Content: Integrated thermal energy from surface to 26o C isotherm:

• Empirical approach to estimate OHC from satellite altimetry (Shay and Brewster, 2010).

• Ocean thermal structure is an important feedback mechanism (Chang and Anthes, 1978).

• Warm core eddies inhibit mixing and provide deep energy source for hurricanes (Shay et al., 2000; Jaimes and Shay, 2009).

MLD

D26

OHC

SST 26°C

dzTcOHCD

zp )26(26

ARGOS, XBT, AXBT, Moorings: 44,000 Profiles From 1998-2009‏ (Meyers et al., 2010)

Tracking Fish Movements with Space-Age Technologies

Ocean Heat Content Empirical Approach (Shay et al. , MWR, 2000)

• Reduced gravity (g’), H20, h (ocean mixed layer depth) GDEM.

• Blend and objectively map SHA from Jason-1, GFO, and Envisat (9.9, 17 and 35-d repeat track).

• Infer H20 using mapped SHA and seasonal climatology.

• Estimate H26 relative to H20 (via ratio).

• Estimate OHC relative to 26oC using H26, h, and SST.

Upper ocean cooling induced by Hurricane Ivan (2004) over the Loop Current (LC) System

Fish Locations Obtained from Satellite-Tag Deployments, 2001-2011

An example blue marlin (Makaira nigricans) movement track derived from satellite-based Popoff Archival Transmitting (PAT) tag deployed between July 3rd to September 29th 2004.

Vertical temperature profile of the blue marlin during the 89 day deployment based on ARGOS transmitted PAT-tag data. The solid black line indicates the depth of 26 oC. White arrow indicates upwelling induced by Hurricane Ivan on September 15th (see Fig. 5).

Ocean Heat Content (OHC, see Fig. 1) derived from the blue marlin’s vertical temperature profile shown above.

Summary • SMARTS improves estimation of OHC in the North Atlantic Ocean basin when combined with

satellite altimetry and SSTs (Meyers, 2011).

• In situ measurements are crucial to improve SMARTS.

• Combining high resolution ABS measurements with improved T,S tags in strong ocean fronts such as the Loop Current and its eddy field provides valuable observations for fisheries and SMARTS.

• A clear connection is emerging between the behaviors of fish and physical oceanographic processes (e.g., 26oC isotherm depth, OHC).

• Need to take the next steps to quantitatively compare satellite-based fields with ABS in situ measurements.

• Assimilating the ABS measurements over the basin will provide key measurements for higher resolution ocean models that will improve coupled biological and physical models for assessing ecosystem stressors (i.e., hurricanes, oil spills, climate changes).

We conclude that by extending the use of Animal Borne Sensors (ABS) data within the existing SMARTS technology framework can greatly improve understanding of the coupled dynamical behaviors of ocean‐atmosphere and fish stock migrations that may portend a new era of forecasting hurricane intensity and novel ecosystem‐based strategies for sustaining key ocean fisheries.

Over the past decade, satellite-based tag technologies have facilitated an improved understanding of migrations, behavior patterns, and environmental preferences for a number of large marine fishes (such as tunas, billfish, sharks, and Atlantic tarpon) providing valuable information for resource managers to ensure protection and sustainability of these valuable and iconic fisheries.

What Do Hurricanes and Tarpon Have in Common? They all prefer SST greater than 26 oC.

Migration track and vertical temperature profile of Tarpon 116

Migration track and vertical temperature profile of Tarpon 86

Daily average temperatures (black dots) and associated monthly frequency distribution (histogram bars).

Distribution of Sea Surface Height field on September 17 from altimetry; warm core eddy (WCE) and cold core eddy (CCE), , relative to the track of Hurricane Ivan. From Halliwell et al. (MWR 2011). Satellite-based SST before (left) and after (right) the passage of Ivan. SST from the HYbrid Coordinate Ocean Model (HYCOM).

Bill. Boyce

Don DeMaria

Acknowledgments Research team from the Upper Ocean Dynamics Laboratory (LKS) gratefully acknowledges support from NOAA NESDIS (NA10OAR4320143) in the development and implementation of SMARTS for Global Ocean Heat Content Project; and NASA Hurricane Science Team (NNX09AC47G) and the NOAA Joint Hurricane Testbed (NA17RJ1226). Fish migration research appreciates the fiscal support from the Bonefish & Tarpon Trust, Robertson Foundation, Sanctuary Friends Foundation of the Florida Keys, Texas Parks & Wildlife Department, Tarpon Tomorrow, Texas Coastal Conservation Association, the Batchelor Foundation, West Coast Inland Navigation District, and Wells-Fargo.

Upwelling

Fig. 1

Fig. 2

Fig. 3

Fig. 4

Fig. 5

Fig. 6

Fig. 7

Atlantic tarpon (Megalops atlanticus)

CCE

WCE CCE

Poster ID: B1173

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