Research Question:  What is the correlation between the location of leatherback sea turtles, sea surface temperature, and chlorophyll?

Data:

Leatherback sea turtle locations: The leatherback turtle dataset was obtained from http://seamap.env.duke.edu/dataset.  The dataset was in point feature format.  The extent of the dataset is within the Gulf of Mexico. Observations of each sea turtle was collected from January through December 2005.

SeaTurtlePointData

Figure 1: Sea turtle locations in the Gulf of Mexico, derived from http://seamap.env.duke.edu/

Sea Surface Temperature: The Sea Surface Temperature (SST) dataset was obtained from NOAA.  The dataset was downloaded from the NOAA website in .csv format with latitude and longitude coordinates and temperature data associated with each coordinate.  The extent of the dataset was the Gulf of Mexico.  The SST data was the average daily maximum for January and December 2005.  The data ranged from 2.44 – 26.89 Celsius, the mean was 23.57 Celsius.

SST_image_GOM

Figure 2: Sea Surface Temperature (Celsius) data for January 2005 within the Gulf of Mexico, derived from NOAA.

Chlorophyll-a: The chlorophyll data was obtained from NOAA.  The dataset was downloaded from the NOAA website in .csv format with latitude and longitude coordinates and chlorophyll data associated with each coordinate.  The extent of the dataset was the Gulf of Mexico.  The Chlorophyll data was a 3-day composite in December 2005.  The data ranged from 0 to 1.63 mg/m3, the mean was 0.29 mg/m3.

Chl_image_GOM

Figure 3: Chlorophyll-a(mg/m^3) data for January 2005 within the Gulf of Mexico, derived from NOAA.

Hypothesis: I expected leatherback sea turtles to be clustered in areas based on high jellyfish concentrations.  Jellyfish tend to be located in areas that have higher chlorophyll-a concentrations and where sea surface temperature is low.  Thus sea turtle locations should correlate well with higher values of chlorophyll-a and lower values of SST.

Analysis Approaches:  To test my hypothesis, I utilized the hotspot analysis, Spatial autocorrelation (Moran’s I), Geographically Weighted Regression, Kernel Density tools in ArcGIS.  In addition, I also utilized R statistical package to create a graph that correlated chlorophyll with SST.

a.  Hotspot Analysis: The spatial distribution of the sea turtle locations appeared to be clustered toward the middle of the Gulf of Mexico.  The hotspot analysis tool helps to identify where statistically significant hotspots or clusters of sea turtles are located within the Gulf of Mexico.

b.  Spatial Autocorrelation (Moran’s I): This tool measures spatial autocorrelation using feature locations and feature values simultaneously. The Moran’s I index will be a value between -1 and 1. Positive spatial autocorrelation will show values that are clustered. Negative autocorrelation is dispersed. Random is close to zero. The tool generates a Z-score and p-value which helps evaluate the significance of the Moran’s index. I tested the spatial autocorrelation of chlorophyll and sea surface temperature at each feature location.  The conceptualization of spatial relationships method used was the inverse distance and the Euclidean distance measure was used for the distance method.  I selected a 500km distance (smaller distances were too small for the study site).

c.  Ordinary Least Squares: This tool performs a global linear regression to “generate predictions or model a dependent variable in terms of its relationships to a set of explanatory variables.  Before conducting this test, I sampled the SST and the CHL-a values at each of the feature locations (sea turtle locations) using the Extract Multi Values to Points tool.  This tool “Extracts cell values at locations specified in a point feature class from one or more rasters, and records the values to the attribute table of the point feature class.”   This model was run three separate times, increasingly adding more explanatory variables each time.  Each OLS run used Chlorophyll as the dependent variable.  The first OLS run, SST as the explanatory variable.  The second run, used SST and depth (m) as the explanatory variables and the third run, used SST, depth, and turtle count as the explanatory variables.

d.  Geographically Weighted Regression: Based on the observations and results found in the OLS analysis (the data being nonstationary).  I decided to conduct a Geographically Weighted Regression analysis.  This tool performs a local form of linear regression used to model spatially varying relationships.  The dependent variable used for this tool was the Chlorophyll and the explanatory variable was SST.

Results:

Hotspot Analysis:  The results of the hotspot analysis (shown below) suggest that the turtle locations are significantly clustered off the coast of Louisiana and Texas between approximately 2000 to 3,000m depth of water.  However, the results of this analysis appear to be quite deceptive.  Upon taking measurements of turtles in the hotspot cluster it appears as though they may be more dispersed.  Further analysis is needed in order to determine further patterns of Sea turtle locations.

hotspotAnalysis_5June

Figure 4: Results of the hotspot analysis for leatherback sea turtle locations

Spatial Autocorrelation (Moran’s I) – sea surface temperature:  The results of the spatial Autocorrelation tool suggest that the pattern of Sea Surface temperature at each feature location is clustered.  The Moran’s Index was 0.402514, the z-score was 2.608211, and the p-value was 0.009102.   Since the critical value (z-score) was greater than 2.58 there is less than 1-percent likelihood that the clustered pattern is a result of random chance.

SeasurfaceTemp_Morans_resullts1Of2 SeasurfaceTemp_Morans_resullts2Of2

Figure 5: Sea surface temperature results for Moran’s I tool.

Spatial Autocorrelation (Moran’s I) – Chlorophyll-a :  The results of the spatial Autocorrelation tool suggest that the pattern of chlorophyll at each feature location is clustered.  The Moran’s Index was 0.346961, the z-score was 2.216243, and the p-value was 0.026675.  The critical value (z-score) was less than 2.58 but greater than 1.96 thus suggesting that there is less than 5-percent likelihood that the clustered pattern is a result of random chance.

Chlorophyll_Morans_resullts1Of2 Chlorophyll_Morans_resullts2Of2

Figure 6:  Results of the spatial autocorrelation Moran’s I for chlorophyll-a at the leatherback sea turtle locations.

Ordinary Least Squares:  This model was run three separate times, increasingly adding more explanatory variables each time.  Each OLS run used Chlorophyll as the dependent variable.  The first OLS run, SST as the explanatory variable.  The second run, used SST and depth (m) as the explanatory variables and the third run, used SST, depth and turtle count as the explanatory variables.

Model 1:

Model Structure:  Chl-a = f(SST)

Model Results:

a) Overall r2: 0.449473

b) Coefficient on SST in model: -0.052654

The results suggest that Chl is negatively related to SST and given the p-value of 0.000, we can deduce that SST is a significant predictor of Chlorophyll-a.

Model 2:

Model Structure:   (Chl =f(SST), (Depth))

Model Structure:

  1. a) Overall r2: 0.452436
  2. b) Coefficient on SST: -0.051769
  3. C) Coefficient on depth: -0.000015

The results suggest that SST and Depth are negatively correlated with Chlorophyll.  Given the p-value of 0.056397 for depth, this is not a statistically significant relationship.  The p-value for SST is 0.0000 suggesting that it is a statistically significant relationship and is a better predictor of chlorophyll-a than depth.

Model 3:

Model Structure:  (Chl =f(SST), (Depth), (Count))

Model Structure:

  1. a) Overall r2: 0.460299
  2. b) Coefficient on SST: -0.050454
  3. c) Coefficient on Depth: -0.000014
  4. d) Coefficient on Count: 0.121644

The results suggest that SST and Depth are negatively correlated with Chlorophyll and the count is positively correlated.  Given the p-value of 0.067482 for depth, this is not a statistically significant relationship.  The p-value for Count is 0.001815, suggesting that the relationship is statistically significant.  The p-value for SST is 0.0000 suggesting that it too is a statistically significant relationship.  In this model we see that the number of turtles found at each location and the SST values have statistically significant relationships to Chlorophyll.  SST has the lowest p-value and would suggest that it is the best indicator for chlorophyll, though we should not discount the count variable.

Overall results: Running the model using three explanatory variables provided the best Overall R-Square value of .46.  The model significance proves to have an overall statistical significance due to the Koenker (BP) statistic being statistically significant, therefore I used the Joint Wald Statistic as an assessor of the model significance.  The Joint Wald Statistic was significant as shown below:

model3_joint_wald_stat

Figure 7: OLS model 3 – Joint Wald Statistic

The Koekner statistic is used to assess model stationarity.  This statistic revealed that the model was not stationary in geographic space and/ or data space due to its significance and having a p-value <0.05 as shown below:

model3_koenker_BP_stat

Figure 8:  OLS model 3 – Koenker BP Statistic

Since the Koekner statistic was significant it was appropriate to look at the robust probabilities of each variable to assess their effectiveness.  The Robust Probability scores for each of variables reveals that the count and SST are statistically significant (as shown below) thus they are found to be important to the regression model.  However, it also appears as though the model is a good candidate for Geographically Weighted Regression due to it being nonstationary.

model3_variable_stats

Figure 9: OLS model 3 – Variable Statistics

 

Geographically Weighted Regression:

Model Structure:  (Chl =f(SST), (Depth), (Count))

Model Result

a) spatial pattern of r2 values (map)

gw2_localr2_update

Figure 10: Geographically Weighted Regression Analysis: Map of the Local R-Squared values

After conducting the GWR analysis using the chlorophyll as the dependent variable and the Sea Surface Temperature as the explanatory variable I mapped the local R-Squared values of each feature location to show where the model predicted well and where it predicted poorly.  The map shows that predicts are made best where turtle locations appear to be in areas where Sea Surface temperature is cooler off the Texas coastline.

b) Spatial pattern of coefficients for SST

GWR_2_coefficients_SST_5June

Figure 11:   Geographically Weighted Regression Analysis: Map of the coefficients

I mapped the coefficients in order to understand regional variation of the model.  When using GWR to model the Chlorophyll (dependent variable) I was interested in understanding the factors that contribute to the turtle locations (or chlorophyll at each of the turtle locations).  I was also interested in examining the stationarity of the data being that the OLS model revealed that it was not stationary.  In order to do these tasks I mapped the coefficient distribution as a surface to show where and how much variation was present.  As shown below in the map, it appears that Sea surface temperature has a negative relationship with Chlorophyll.  The range of the coefficients is -0.066176 to -0.64989.  There is very little variation in the coefficients.  The results of this test help to inform policies at a regional scale.

Significance: What did you learn from your results?  How are these results important to science? to resource managers?

The results of the tests suggest that chlorophyll-a has a negative relationship to sea surface temperature in the Gulf of Mexico according to leatherback sea turtle locations.  Sea turtles are located in areas where sea surface temperature is low and chlorophyll values are higher.  After mapping the coefficients of the variables we see that there is little variation in the data suggesting that policies regarding the protection of leatherback sea turtles should extend throughout the entirety of the Gulf of Mexico rather than in a few selected areas.

Learning Outcomes:

Programming in R:

With the help of Mark Roberts, I was able to use the R software programming to load and utilize the ggplot2 package to plot the correlation between chlorophyll-a and sea surface temperature. Lots of room for improvement here!  The following is the code used to make the plot as well as the plot outcome:

GGplot_code

Figure 12: ggplot code used in R to plot the correlation between chlorophyll-a and sea surface temperature.

 

Chlorophyll_vs_SST_plot

Figure 13: Correlation between chlorophyll-a and sea surface temperature.

 

What did you learn about spatial statistics:

I think scale is an important factor.  You need to understand your data and be sure to not take the results as they are.  You should investigate everything to make sure that the data and results make sense.  If the results appear incorrect they probably are incorrect.   I also  learned that it is dangerous to conduct spatial statistical analyses on data unless you can interpret what makes sense. The spatial autocorrelation conducted on SST and Chl-a indicated that they were clustered but I was still confused about this outcome.  While conducting research it is important to thing about scale of the data to ensure that all of the data line up.  I encountered an issue with the SST data due to the way it was sampled. I had many sea turtle locations that did not have sea surface data associated with them because of the way the SST data was sampled.   A classmate pointed out that I did not consider the effects of currents on jellyfish.  This could be a significant factor that may lead us to understand why sea turtles are present in Gulf of Mexico since jellyfish are partially distributed by currents.  Another lesson learned is that it is important to remember the basic principles of geographic information systems while conducting these analyses.  For instance it is important to turn on extensions, and be sure that all the data is properly projected prior to conducting any analysis as this can and will through off the results. Overall, it is important to know your data.

 

Spatial Autocorrelation (Moran’s I): This tool measures spatial autocorrelation using feature locations and feature values simultaneously.   The spatial autocorrelation tool utilizes a multidimensional and multi-directional factors.  The Moran’s I index will be a value between -1 and 1. Positive spatial autocorrelation will show values that are clustered. Negative autocorrelation is dispersed. Random is close to zero. The tool generates a Z-score and p-value which helps evaluate the significance of the Moran’s index.

Morans_Calculations

Figure 1: Calculations used for the Moran’s I tool. (ESRI image)

The output of the Moran’s I tool can be found in the results section of ArcGIS.  Upon opening the HTML report for the Moran’s I results you will see a graph showing how the tool calculated the data and whether or not the data is dispersed, random, or clustered.  This report will also include the Moran’s Index value, z-score, p-value.  It will also provide a scale for the significance of the p-value and critical value for the z-score.

MoransI_SampleOutput

Figure 2: Sample output for the Moran’s I tool. (ESRI image)

 

Data and Analysis

Before conducting this test, I sampled the SST and the CHL-a values at each of the feature locations (sea turtle locations) using the Extract Multi Values to Points tool. This tool “Extracts cell values at locations specified in a point feature class from one or more rasters, and records the values to the attribute table of the point feature class.”

SeaTurtlePointData

Figure 3: Sea turtle locations in the Gulf of Mexico, derived from http://seamap.env.duke.edu/

 

Chl_image_GOM

Figure 4: Chlorophyll-a(mg/m^3) data for January 2005 within the Gulf of Mexico, derived from NOAA.

SST_image_GOM

Figure 5: Sea Surface Temperautre (Celsius) data for January 2005 within the Gulf of Mexico, derived from NOAA.

I tested the spatial autocorrelation of chlorophyll-a and sea surface temperature at each feature location.  The conceptualization of spatial relationships method used was the inverse distance and the Euclidean distance measure was used for the distance method.  I selected a 500km distance (smaller distances were too small for the study site).

Results:

Sea Surface Temperature: The results of the spatial autocorrelation tool suggest that the pattern of sea surface temperature at each feature location is clustered. The Moran’s Index was 0.402514, the z-score was 2.608211, and the p-value was 0.009102.  Since the critical value (z-score) was greater than 2.58 there is less than 1-percent likelihood that the clustered pattern is a result of random chance.

SeasurfaceTemp_Morans_resullts1Of2 SeasurfaceTemp_Morans_resullts2Of2

Figure 6: Sea surface temperature results for Moran’s I tool.

Chlorophyll-a :  The results of the spatial Autocorrelation tool suggest that the pattern of chlorophyll at each feature location is clustered.  The Moran’s Index was 0.346961, the z-score was 2.216243, and the p-value was 0.026675.  The critical value (z-score) was less than 2.58 but greater than 1.96 thus suggesting that there is less than 5-percent likelihood that the clustered pattern is a result of random chance.

Chlorophyll_Morans_resullts1Of2 Chlorophyll_Morans_resullts2Of2

Figure 7: Results of the spatial autocorrelation Moran’s I for chlorophyll-a at the leatherback sea turtle locations.

What does this mean:

As suggested in the hotspot analysis there is clustering of the data.  The spatial autocorrelation tool indicates that clustering is occurring with regard to the sea surface temperature and chlorophyll values at their respective locations with regard to sea turtles.   Conducting an ordinary least squared analysis may lead to more information about which factors contribute more to the clustered pattern.

Introduction:  Leatherback sea turtles are endangered world wide.  Their habitat is often impeded due to the oil and gas industry in the Gulf of Mexico.  In 2010, the Deepwater Horizon Oil Spill affected much of the biota when 200million gallons of oil spilled into the Gulf.  Leatherback sea turtles are the most endangered sea turtle. My research  question is focused on the extent to which these turtles utilize the Gulf of Mexico.  Leatherback sea turtles feed almost exclusively on jellyfish. I will be assessing their range by looking at the correlation between leatherback sea turtle point data, sea surface temperature and chlorophyll as proxies for where jellyfish may occur.

„Research Question: What is the correlation between the location of leatherback sea turtles, sea surface temperature, and chlorophyll?

Approach: I used the hotpsot analysis tool in order to explore the sea turtle point data.  the hotspot analysis tool identify where statistically significant hotspots or clusters of sea turtles are located within the Gulf of Mexico.

Sea turtle data:

SeaTurtlePointData

 

Results:  The results of the hotspot analysis (shown below) suggest that the turtle locations are significantly clustered off the coast of Louisiana and Texas between approximately 2,000m to 3,000m depth of water.  However, the results of this analysis appear to be quite deceptive.  Upon taking measurements of turtles in the hotspot cluster it appears as though they may be more dispersed.  Further analysis is needed in order to determine further patterns of sea turtle locations.

hotspotAnalysis_5June

Question:

What was the effects of the DWH oil spill and associated response activities (e.g. 200 million gallons of oil, 1.8 million gallons of dispersant, in situ burns, and hundreds of additional boats) on the foraging behavior of approximately 1000 sperm whales residing in the Gulf of Mexico?  Sperm whales are extremely efficient deep-diving marine predators, tending to feed on patches of prey that they locate with a mixture of clicks and creaks (Watwood et al. 2006). Dive profile records indicate that sperm whales in the Gulf of Mexico forage near 520 m depth in the water column (Watwood et al. 2006). Sperm whales feed along and about the 1000-m isobath in the region between Mississippi Canyon and De Soto Canyon (Jochens et al. 2008) (Figure 1.). They may consume several thousand kilograms of prey a day (Best 1979) comprised of about 1000 individuals (Clarke et al. 1997). Given their food consumption needs, their prey resources are likely a critical factor driving their distribution and foraging behavior in the Gulf of Mexico during the spill.

Datasets:

I have requested satellite tag data form Oregon State University Marine Mammal Institute. Fortunately, OSU scientists tagged and tracked sperm whales prior to the spill, during, and after. However, there is a good chance I will need to change projects because I do not currently have datasets for analyses.

Hypotheses:

I hypothesize that the availability of sufficient prey resources required to meet the caloric needs of resident sperm whales outweighed the chaos created by the oil spill and response activities.

Approaches:

I am not sure of the best approach, but hope to get some assistance from my peers. My goal is to measure any shift in foraging areas and to complete trend analysis, hot spot analysis, and cluster analysis of foraging areas prior to, during, and several years post spill.

Expected Outcomes:

It would be ideal to detect patterns that are predictive of food web disturbance that ultimately predict the response to sperm whales to disturbance.

Level of preparation:

I have moderate experience with ArcMap and some experience with spatial analyses with ArcMap. I have an understanding of basic statistics and statistical software Minitab. I do not have any experience with R or Python.

References:

Best, P.B. 1979. Social organization in sperm whales, Physeter macrocephalus. Pp. 227-289 in Behavior of marine animals, Vol. 3, edited by H.E. Winn and B.L. Olla. Plenum, New York.

Clarke, M.R. 1997. Cephalopods in the stomach of a sperm whale stranded between the islands of Terschelling and Ameland, southern North Sea. Bulletin de 1’Institut Royal des Sciences Naturelles de Belgique, Biologic 67-Suppl 53-55.

Jochens, A.E. and D.C. Biggs, editors. 2006. “ Sperm whale seismic study in the Gulf of Mexico; Annual Report: Years 3 and 4.” OCS Study MMS 2006-067. 111 pp., Minerals Management Service, Gulf of Mexico OCS Region, U.S. Dept. of the Interior, New Orleans, LA.

Jochens, A., D. Biggs, K. Benoit-Bird, D. Engelhaupt, J. Gordon, C. Hu, N. Jaquet, M. Johnson, R. Leben, B. Mate, P. Miller, J. Ortega-Ortiz, A. Thode, P. Tyack, and B. W. 2008. 2008. “Sperm whale seismic study in the Gulf of Mexico: Synthesis report.” OCS Study MMS 2008-006. 341 pp, Minerals Management Service, Gulf of Mexico OCS Region, U.S. Dept. of the Interior, New Orleans, LA.

Watwood, S.L., P.J. Miller, M. Johnson, P.T. Madsen, and P.L. 2. Tyack. 2006. Deep‐diving foraging behaviour of sperm whales (Physeter macrocephalus). Journal of Animal Ecology 75(3):814-825.