Supplementary Materials for

Size: px
Start display at page:

Download "Supplementary Materials for"

Transcription

1 Supplementary Materials for Direct quantification of energy intake in an apex marine predator suggests physiology is a key driver of migrations Rebecca E. Whitlock, Elliott L. Hazen, Andreas Walli, Charles Farwell, Steven J. Bograd, David G. Foley, Michael Castleton, Barbara A. Block This PDF file includes: Published 11 September 2015, Sci. Adv. 1, e (2015) DOI: /sciadv Fig. S1. Spatial plot of the data set analyzed in this paper by month. Fig. S2. Raw data (visceral temperature, red line; ambient temperature, blue line) trace from an archival tagged Pacific bluefin tuna. Fig. S3. Raw data (visceral temperature, red line; ambient temperature, blue line) trace from a second archival tagged Pacific bluefin tuna. Fig. S4. Tracks with estimated median HIF (kcal day 1 ) for two archival tagged Pacific bluefin tuna. Fig. S5. Correlates of average daily energy intake (kcal) in tagged Pacific bluefin tuna. Fig. S6. HIF in relation to SST, latitude, and chl-a. Fig. S7. Predicted values for weekly mean thermal excess ( C) plotted by quarter from the final GAMM fitted to thermal excess data between 2002 and 2009 (data from 144 archival tagged Pacific bluefin tuna with 5961 weekly values of thermal excess). Fig. S8. Patterns of habitat use and energy intake by length for archival tagged Pacific bluefin tuna between 2002 and Fig. S9. Physiological responses to ambient temperature with mean energy intake. Fig. S10. Boxplot of posterior predictive probability distributions for estimated energy intake (kcal) for three archival tagged Pacific bluefin tuna in the feeding experiment (22). Fig. S11. Histograms of HIF magnitude observations. Fig. S12. Estimated smooth terms from the GAMM for feeding success in archival tagged Pacific bluefin tuna.

2 Fig. S13. Predicted feeding success between September 2002 and August 2003 from the binomial GAMM for a subset of archival tagged Pacific bluefin tuna (23 tagged individuals, 6705 observations) released in August Fig. S14. Predicted HIF magnitude (conditional on feeding on a given day) between September 2002 and August 2003 from the Gamma GAMM for a subset of archival tagged Pacific bluefin tuna (23 tagged individuals, 6212 observations) released in August Fig. S15. GAMM-predicted values from the delta-gamma model for HIF magnitude (combining predictions of feeding success and HIF magnitude) between September 2002 and August 2003 for a subset of archival tagged Pacific bluefin tuna (23 tagged individuals, 6212 observations) released in August Table S1. Proximate analysis of sardine and anchovy used as feeds for captive tuna, reproduced from Farwell (43). Table S2. Priors in the hierarchical Bayesian regression model. Table S3. Wilcoxon rank sums (from two-sided tests) for size-based differences in latitude, SST, and HIF. Table S4. Correlates of thermal excess. References (36 43)

3 Supplementary Figures Figure S1. Spatial plot of the data set analyzed in this paper by month. Each yellow circle marks one daily geolocation point for an archival-tagged Pacific bluefin tuna.

4 Figure S2. Raw data (visceral temperature, red line; ambient temperature, blue line) trace from an archival tagged Pacific bluefin tuna. Panels A-C show one year of data (1 st January to 31 st December 2003), while panels D-F show one week of data from the corresponding 4-month period plotted in A-C. The green line shows the model predicted baseline visceral temperature (i.e. with no feeding), while the grey shaded area indicates HIF area as quantified by the model. This individual was at approximately 29 N at during the first period with few feeding events (8 th to 25 th August); it reached a latitude of 38 N in mid-september, having been at 23 N in early June. The second period with little feeding is associated with a southward movement the individual was at 38 N on 28 th October, and moved south to N, where few feeding events were observed (13 th -30 th November) after this, it moved north again, reaching 34 N by mid-december.

5 Figure S3. Raw data (visceral temperature, red line; ambient temperature, blue line) trace from a second archival tagged Pacific bluefin tuna. Panels A-C show one year of data (1 st January to 31 st December 2003), while panels D-F show one week of data from the corresponding 4-month period plotted in A-C. The green line shows the model predicted baseline visceral temperature (i.e. with no feeding), while the grey shaded area indicates HIF area as quantified by the model. Periods with few feeding events occurred between 9 th and 22 nd August, when the fish was migrating northwards (between 30 N and 32 N) and between 1 st and 16 th November, again between approximately 30 N and 32. Prior to this (mid-october) the fish was at 35 N; it moved northwards again in late November, reaching 33 N by the end of November.

6 Figure S4. Tracks with estimated median HIF (kcal day -1 ) for two archival tagged Pacific bluefin tuna. Panels A and B show daily median HIF (kcal) between April and October in 2003 (A) and 2004 (B) for the same individual. Panels C and D show daily median HIF (kcal) between April and October in 2003 (C) and 2004 (D) for a second tagged individual. Latitudes for the first HIF in April are between 24.6 N and 24.8 N in all panels (i.e. fish are moving northwards). The radius of the

7 circles is proportional to estimated median HIF magnitude on a given day. HIF magnitude is also indicated by the colour scale. Figure S5. Correlates of average daily energy intake (kcal) in tagged Pacific bluefin tuna. Estimated response curves (smooth terms) and year effects from the final generalized additive mixed model. Panel (A) eddy kinetic energy; (B) relative light level; (C) day of the year; (D) year. Dashed lines represent 95% confidence limits. Vertical axes in A-D are partial responses (estimated, centered smooth functions) on the scale of the linear predictor.

8 Figure S6. HIF in relation to SST, latitude, and chl-a. (A) Latitudinal distribution of tagged bluefin tuna in the California Current. Top, latitude versus date with mean daily SST ( C) recorded by the tags indicated by the colour scale. Centre, Hovmöller plot for predicted daily energy intake (kcal) from 2003 to Bottom, Hovmöller plot for the logarithm of the median daily chlorophyll-a concentration (mg m -3 ) from the SeaWifs and MODIS sensors. The solid black line in each panel denotes median latitude, while the dashed lines show the 2.5th and 97.5th percentiles for the latitudinal distribution. (B) Median plus 2.5 and 97.5 percentiles for SST (obtained from archival tags) over the course of the year.

9 Figure S7. Predicted values for weekly mean thermal excess ( C) plotted by quarter from the final GAMM fitted to thermal excess data between 2002 and 2009 (data from 144 archival tagged Pacific bluefin tuna with 5961 weekly values of thermal excess). (A) September to November (B) December to February (C) March to May (D) June to August.

10

11 Figure S8. Patterns of habitat use and energy intake by length for archival tagged Pacific bluefin tuna between 2002 and (A) Utilisation densities for archival tagged Pacific bluefin tuna in the California Current in February - solid line, 50% density contour; dashed lines, 10% and 90% density contours. (B) Observed energy intake (interpolated and smoothed for visualisation) by time and latitude in January and February. (C) Utilisation densities for archival tagged Pacific bluefin tuna in the California Current in October - solid line, 50% density contour; dashed lines, 10% and 90% density contours. (D) Observed energy intake (interpolated and smoothed for visualisation) by time and latitude October and November. In each panel, age increases from left to right: left, age 2.5 years and younger; centre, age years; right older than 3.5 years.

12 Figure S9. Physiological responses to ambient temperature with mean energy intake. Black, rate of oxygen consumption, MO2, of bluefin tuna swimming at a constant speed of 1.0 body length per second (mg kg -1 h -1, mean ± 1 SD, N=6); grey (with dashed line), heart rate [beats min -1, mean ± 1 SE, N=4 (10, 20, 25 ), N=6 (15 )]; orange, energy intake (kcal) in wild bluefin tuna, mean +/- 1 SE. The histogram shows the number of days spent by archival tagged Pacific bluefin tuna in each 1 C temperature bin (N=39,387 days).

13 Figure S10. Boxplot of posterior predictive probability distributions for estimated energy intake (kcal) for 3 archival tagged Pacific bluefin tuna in the feeding experiment 22. Each box summarises the posterior predictive distribution for one feeding; horizontal lines through the centre of each box denote the median, while the ends of the box denote the upper and lower quartiles. Whiskers denote the 95% probability interval. Feedings are shown in order of ascending estimated energy intake. Blue boxes, normal observation model 22 ; black boxes, lognormal observation model (this study). Supplementary Methods Hierarchical Bayesian regression model (HBM) We apply a slightly modified version of the hierarchical Bayesian model (HBM) to quantify the relationship between meal energy and HIF area 22 that uses a lognormal observation model to estimate daily HIF magnitude as a function of peritoneal and ambient temperature in wild Pacific bluefin tuna. Prior distributions (summarising knowledge about the parameter before making

14 experimental observations) for parameters whose prior is not given below can be found in Supplementary Table S2. In the equations that follow, Normal distributions are parameterized in terms of mean and variance. Equations are given on a logarithmic scale unless otherwise stated. Vague normal priors were placed on the means of the population level priors for regression coefficients for squid and sardine feeds at 20 C: S [20] ~ Normal (0,5 ), S [20] ~ Normal (0,5 ), where ~ means is distributed as, 1 [20] denotes the mean of the population level prior for squid feeds at 20 C and 2 [20] denotes the mean of the population level prior for sardine feeds at 20 C. Individual level regression coefficients at 20 C were assumed to arise from a common (population level) normal distribution with means given above and food type-specific standard deviations: 2 S3. 1,i Normal [20] 1 [20] 1, [20] ~ (, ), 2 S4. 2, i Normal [20] 2 [20] 2 [20] ~ (, ),

15 where 1, i[20] is the squid feed regression coefficient for individual i at 20 C and 2, i [20] is the 2 2 sardine feed regression coefficient for individual i at 20 C. and are the variances of the [20] [ 20] population level priors for log-scale regression coefficients at 20 C, for squid and sardine feeds respectively. 1, 2, A vague normal prior was placed on the mean of the population level prior for the ratio of the slope of kcal/hif magnitude at 20 C to the slope of kcal/hif magnitude at 15 for squid feeds, : 1,1 2 S5. ~ Normal (0,3.16 ), 1,1 Log-scale individual level priors for temperature effect parameters for squid feeds (slopes at 15 C relative to 20 C), i,1,1, were assumed to arise from a common (population level) normal distribution with mean given above:, 2 S6. i,1,1 ~ Normal (, ) 1,1 where i,1,1 is the temperature effect parameter for individual i for squid feeds at 15 C relative to 2 20 C and is the variance of the population level prior for the temperature effect parameter for squid feeds at 15 C relative to 20 C. Priors for the individual level temperature effect parameters for squid feeds at 22 C relative to 20 C were specified relative to those for 15 C relative to 20 C as:

16 , S7. i,1,2 i,1,1 where i,1,2 is the temperature effect parameter for individual i for squid feeds at 22 C relative to 20 C and: S8. 2 ~ Normal (0,31.62 ). Similarly, priors for log-scale temperature effect parameters for sardine feeds were specified relative to the log-scale temperature effect parameters for squid feeds:, S9. i,2,1 i,1,1 1, S10. i,2,2 i,1,2 2 where i,1,2 is the temperature effect parameter for individual i for sardine feeds at 15 C relative to 20 C and i,2,2 is the temperature effect parameter for individual i for sardine feeds at 22 C relative to 20 C. γ parameters were given vague normal priors (Table S2). Priors for log-scale individual level regression coefficients at 15 C and 22 C were expressed relative to the log-scale individual level coefficient priors at 20 C (equations S11 to S14):

17 S11. 1, [15] 1,i [20],1,1 log( ), i i S12. 1, [22] 1,i [20],1,2 log( ), i i S13. 2,i [15] 2,i [20] i,2,1 log( ), S14. 2,i [22] 2,i [20] i,2,2 log( ), Predicted meal energy (kcal) for squid and sardine feeds, respectively, is then given by: yˆ log( ), S15. 1, i, j, k 1, i, k 1, i, j, k yˆ log( ), S16. 2, i, j, k 2, i, k 2, i, j, k where 1, i, j, k is HIF magnitude ( C hours) for squid feed j for individual i at temperature level k and y ˆ1, i, j, k is the log-scale predicted meal energy in kcal for squid feed j for individual i at temperature level k (equation S15) and analogously for sardine feeds (equation S16). k=1 denotes feedings at 15 C;. k=2 denotes feedings at 20 C and k=3 denotes feedings at 22 C. Log-transformed measured meal energy values (kcal) for squid and sardine were assumed to be normally distributed around the predicted energetic value for a given individual, food type and tank temperature:

18 S17. log( y ) ~ Normal ( yˆ, ), 2 1, i, j, k 1, i, j, k obs,1 S18. log( y ) ~ Normal ( yˆ, ), 2 2, i, j, k 2, i, j, k obs,2 where y 1, i, j, k is the measured caloric value of squid feed j for fish i at temperature level k, and y 2, i, j, k is the measured caloric value of sardine feed j for fish i at temperature level k. 2 obs,2 are observation error variances for squid and sardine feeds, respectively. 2 obs,1 and To obtain an estimate of energy intake in a wild juvenile Pacific bluefin tuna for which no experimental observations are available, the posterior predictive distribution is used. The posterior predictive distribution can be obtained by sampling random effect parameters from their respective distributions, given the posteriors for hyperpriors, e.g. assuming a diet of sardine: 2 S19. 2, i Normal [20] 2 [20] 2 [20] ' ~ (, ), 2 S20. ' i,1,1 ~ Normal (, ) 1,1, ' ', S21. i,2,1 i,1,1 1 ' ', S22. i,2,2 i,1,1 2 where the prime sign indicates a new individual i. The resulting sampled parameters can then be used to obtain the regression coefficient for a given measured SST:

19 ' ' (1 I ) ' (19.9 SST ) I ' ( SST 19.9), S23. 2, i SST 2, i [20] T i,2,1 T i,2,2 where IT is an indicator variable taking a value of 0 for SST 19.9 C and 1 for SST> 19.9 C. The SSTspecific regression coefficient for a new individual ( 2, i used to predict (log) energy intake (kcal) for HIF event j: ' SST ) and the observed HIF magnitude are yˆ ' log( ). S24. 2, i, j SST 2, i SST i, j The posterior predictive distribution for energy intake (kcal) (assuming a diet of sardine) takes into 2 account the estimated observation error variance, obs,2: S25. log( y ) ~ Normal ( yˆ, ). 2 2, i, j SST 2, i, j SST obs,2 Assumptions about diet in wild Pacific bluefin tuna The results presented in this paper assume a diet of sardines (Sardinops sagax) or forage fish of similar nutritional composition 22,36. While the use of one food type is a simplification, sardines have been found to comprise the main food item for Pacific bluefin tuna in the eastern Pacific Ocean in an earlier study 36. Analysis of the stomach contents of 650 Pacific bluefin tuna

20 caught off southern California and Baja Califonia between 1968 and 1969 showed that forage fish constitute 91.8% by number and 93.1% by volume of all food consumed 36. Northern anchovy (Engraulis mordax) was the most important food item, comprising 86.6% by number and 80.0% by volume of the bluefin diet 36, while cephalopods comprised 3.88% by number and 2.16% by volume. S. Sagax and E. mordax are comparable in terms of their nutritional compositions (Table S1). A study from 2007 hypothesized that Pacific bluefin tuna in the eastern Pacific would primarily have consumed S. sagax in recent years 9. This was based on observations from a tagging cruise in 2002, which revealed that most of the bluefin tuna had Pacific sardines in their stomachs 9. In a more recent study Pacific bluefin tuna were found to show a high degree of omnivory, with a trophic group containing S. sagax making up around a third of the diet, although the seasonal and spatial coverage of this study was more limited 36,37. Assuming a fixed proportion of squid (or other prey items with differing nutritional values) and sardine in the diet across regions and seasons would not be expected to lead to different predictions about relative energy intake in time and space, although absolute values would change. More problematic is the possibility that juvenile bluefin exploit different prey resources in different areas of their distribution. Differences in prey energy content alone would not be expected to lead to marked differences in predictions, as we accounted for the caloric densities of food items in the laboratory experiments used to estimate the relationship between energy intake and HIF 22. However, if Pacific bluefin switch between prey items with markedly differing protein contents in different areas of their distribution, our model may under- or over- estimate HIF in some regions. Seasonal collection of stomach content samples at a range of locations would allow development of the model to accommodate this behavior.

21 GAMM for daily HIF Appropriate error distributions for response variables (estimated daily energy intake and thermal excess) were selected by plotting histograms and then using maximum likelihood methods to select among suitable candidate distributions for the resulting frequency distribution. Inspection of the daily HIF data revealed a fairly high proportion of days with no feeding (i.e. zero-inflated data, Figure S11), suggesting that a two-step modeling approach was appropriate. We chose to combine a Bernoulli model for the presence or absence of HIF on a given day with a suitable model for HIF magnitude (conditional on a non-zero observation). For purposes of analysis, days with total HIF of 50 kcal or less were also counted as non-feeding days or zeros. A gamma density was found to be a suitable error distribution for positive-valued HIFs on the basis of likelihoods computed for different parametric distributions (Figure S11), so that the overall model for the distribution is a Delta-Gamma model 38. The likelihood for all HIF observations is given by (equation S26): S26. L(y) (1 p) n m p m y 0 y e ( r)( / r) r 1 ry/ r where Ly ( ) denotes the likelihood of the data, n denotes the total number of data, and m denotes the number of successes in the binomial distribution (here, the number of days with HIF events). The gamma density is expressed in term of its mean and shape parameter r. To implement this error structure in Generalized Additive Mixed Models, a binomial GAMM with logit link was used to model the numbers of zero and non-zero data, and a GAMM with Gamma

22 distributed error and a log link was used to model positive valued data. Fitted mean values for a given set of covariates can then be obtained by multiplying the probability of feeding (p) from the binomial GAMM with predicted HIF magnitude, conditional on feeding ( ) from the Gamma GAMM Figure S11. Histograms of HIF magnitude observations. (A) all observations. (B) positive-valued observations, with parametric distributions fitted by maximum likelihood indicated; red, gamma distribution; blue, lognormal distribution. We applied GAMMs to the daily feeding success and HIF magnitude data for a subset of archival tagged juvenile Pacific bluefin tuna released in August 2002 (those with tracks of at least 300 days)

23 over their first year at large (n=6705; 23 tagged individuals). We used R package gamm4 (version ) to fit the binomial model for feeding success as it offers better performance for binary data. R package mgcv (version ) was used to fit GAMMS for the magnitude of positive valued HIFs. Supplementary Results Over their first year at large, juvenile Pacific bluefin tuna released in August 2002 fed on 92% of days (SE 0.3%). Feeding success was higher on days when successful feeding had occurred on the previous day (lag 1 autocorrelation =0.35; Durbin Watson test statistic=1.29; P < 0.01). A GAMM for daily feeding success during the first year at large of archival tagged Pacific bluefin tuna released in August 2002 with individual as a random effect, binomial error and a logit link function explained 23% of the total variation (adjusted R-squared) in feeding success. The final model included SST, relative light level, ILD and day of the year as predictors of feeding success (Figure S12). Seasonal and spatial variation in GAMM predicted feeding success is shown in Figure S13. On average, feeding success was predicted to be highest in spring (0.97 ± (SE) and summer (0.92 ± 0.007), with lower feeding success in autumn (0.90 ± 0.008) and winter (0.91 ± 0.006). In winter, lower feeding success was predicted off northern Baja California and north of Cedros Island (Figure S13). By spring, feeding success was predicted to be high in all areas of the tuna s distribution. Slightly lower feeding success was predicted in the southern California Bight and off northern Baja California in summer, while in autumn, the highest feeding success was predicted in the northern part of the tuna s range off central and northern California (Figure S13).

24 Figure S12. Estimated smooth terms from the GAMM for feeding success in archival tagged Pacific bluefin tuna. (A) sea surface temperature (B) mixed layer depth (C) relative light level (D) day of the year. Dashed lines represent 95% confidence limits. Vertical axes are partial responses (estimated, centered smooth functions) on the scale of the linear predictor. A GAMM for daily HIF magnitude when successful feeding occurred with individual as a random effect explained 23% of the total variation in the magnitude of positive-valued HIFs. The final model included relative light level, ILD, day of the year, location (latitude-longitude smooth) and length of the individual as predictors of HIF magnitude. An AR1 error structure (nested within

25 individual) was also found to provide a better fit to the daily HIF magnitude data (lower AIC value) compared with a model without correlation in errors. The correlation parameter estimate for daily HIF was 0.42 (interval ). Considering only days on which feeding occurred (results from the Gamma GAMM), the highest energy intake was predicted in summer (June to August) followed by winter (December to February), Figure S14. Accounting for feeding success too (by combining predictions from the binomial and Gamma GAMMs), the highest average energy intake was predicted in summer, followed by spring (March to May). In winter and spring, when feeding occurred, higher energy intake was predicted at the northern end of the tuna s distribution, off central California and to a lesser extent, off Punta Eugenia in spring (Figure S14). Some individuals made westward movements in winter or spring before moving east again to rejoin the main area of aggregation (Figure S1). These movements often appeared to be associated with high caloric intake (Figures S14, S15). In summer, predicted energy intake was highest in areas closest to the coast in the southern California Bight and off northern Baja California. By autumn, higher energy intake was again predicted at the northern end of the tuna s distribution, off northern California. A similar pattern was obtained from the Delta-Gamma model, when predictions of feeding success and HIF magnitude (conditional on feeding) were combined (Figure S15).

26 Figure S13. Predicted feeding success between September 2002 and August 2003 from the binomial GAMM for a subset of archival tagged Pacific bluefin tuna (23 tagged individuals, 6705 observations) released in August (A) September to November (B) December to February (C) March to May (D) June to August.

27 Figure S14. Predicted HIF magnitude (conditional on feeding on a given day) between September 2002 and August 2003 from the Gamma GAMM for a subset of archival tagged Pacific bluefin tuna (23 tagged individuals, 6212 observations) released in August (A) September to November (B) December to February (C) March to May (D) June to August.

28 Figure S15. GAMM-predicted values from the Delta-Gamma model for HIF magnitude (combining predictions of feeding success and HIF magnitude) between September 2002 and August 2003 for a subset of archival tagged Pacific bluefin tuna (23 tagged individuals, 6212 observations) released in August (A) September to November (B) December to February (C) March to May (D) June to August.

29 Abbreviations CCLME CFL GAM GAMM HIF HBM ILD SD SE SST California Current Large Marine Ecosystem Curved fork length Generalised additive model Generalised additive mixed model Heat increment of feeding Hierarchical Bayesian model Isothermal layer depth Standard deviation Standard error Sea surface temperature Supplementary References 36. Pinkas, L., Oliphant, M. S. & Iverson, I. L. K. Food habits of Albacore, Bluefin tuna, and Bonito in California Waters. California Department of Fish and Game Fish Bulletin 152 (1971). 37. Madigan, D.J. et al. Stable isotope analysis challenges wasp-waist food web assumptions in an upwelling pelagic ecosystem. Sci.Rep. 2, DOI: /srep00654 (2012). 38. Stefánsson, G. Analysis of groundfish surey abundance data: combining the GLM and delta approaches. ICES J. Mar. Sci. 53, (1996). 39. Pennington, M. Efficient estimators of abundance, for fish and plankton surveys. Biometrics, 39, (1963).

30 40. Barry, S.C., Welsh, A.H. Generalized additive modeling and zero-inflated count data. Ecol. Model. 157, (2002). 41. Wood, S., Scheipl, F. gamm4: Generalized additive mixed models using mgcv and lme4. R package version (2013). 42. Wood, S.N. Fast stable restricted maximum likelihood and marginal likelihood estimation of semiparametric generalized linear models. J. Royal Stat. Soc. B 73, 3-36 (2011). 43. Block, B. A. and Stevens, E. D. Tuna: Physiology, Ecology, and Evolution, San Diego: Academic Press (2001).

31 Table S1. Proximate analysis of sardine and anchovy used as feeds for captive tuna, reproduced from Farwell (43). Species Sardinops sagax Engraulis mordax Size Small (35g) Large (75g) Small (11g) Large (34g) Percent protein Percent fat kcal/100g

32 Table S2. Priors in the hierarchical Bayesian regression model. Parameter Description Prior Hyperprior mean for the per degree proportion of the 1,1 slope of kcal/hif magnitude at 20 C the slope of Normal (0,10) kcal/hif magnitude at 15 C represents (squid feeds) Hyperprior standard deviation for the per degree proportion of the slope of kcal/hif magnitude at 20 C the slope of kcal/hif magnitude at 15 C represents Uniform(0.0001, 2) (squid feeds) Multiplier for the temperature effect between 20 C to 22 C relative to 15 C to 20 C for squid feeds. Normal (0,1000) Multiplier for the temperature effect between 15 C 1 and 20 C for sardine feeds relative to the temperature Normal (0,1000) effect for squid feeds. Multiplier for the temperature effect between 20 C 2 and 22 C for sardine feeds relative to the temperature Normal (0,1000) effect for squid feeds. 1 [20] Hyperprior standard deviation for the squid feed coefficient at 20 C. Uniform(0.0001, 2)

33 2 [ 20] Hyperprior standard deviation for the sardine feed coefficient at 20 C. Uniform(0.0001, 2) obs,1 Observation error standard deviation for logtransformed meal energy (kcal), squid feeds Uniform(0.0001,1) obs,2 Observation error standard deviation for logtransformed meal energy (kcal), sardine feeds Uniform(0.0001,1) Parameters of normal distributions are mean and variance.

34 Table S3. Wilcoxon rank sums (from two-sided tests) for size-based differences in latitude, SST, and HIF. Latitude Temperature HIF magnitude Month Age 2 and younger vs. age 3 Age 3 vs. age 4 and older Age 2 and younger vs. age 3 Age 3 vs. age 4 and older Age 2 and younger vs. age 3 Age 3 vs. age 4 and older *** *** *** *** *** * *** *** ** ** ** ** *** *** *** *** *** *** *** *** *** *** *** * *** *** *** *** *** * *** ** 75761*** *** ** *** * *** *** *** *** *** *** *** *** *** *** ** *** *** *** *** * ** * *** ***

35 The significance of comparisons of the distributions of latitude ( ), SST ( C) and the magnitude of the heat increment of feeding (kcal) is denoted by asterisks: * P < 0.05; **P<0.01; ***P< The colour of the cell indicates the direction of significant differences: red indicates a higher value of the variable in question for the younger age class, while blue indicates a lower value for the younger age class. See Methods for age class definitions.

36 Table S4. Correlates of thermal excess. GAMM term Approximate percentage deviance explained Approximate significance level s(sea surface temperature, C) 59% p<0.001 s(isothermal layer depth, m) 3% p<0.001 s(eddy kinetic energy, cm 2 s -2 ) 3% p<0.001 s(sea surface height anomaly, cm) 3% p<0.001 s(relative light level) 3% p<0.001 s(length, cm) 12% p<0.001 s(day of the year) 12% p<0.001 Entries are approximate percentage deviance explained by term (of the total deviance explained by the model) for the final Generalized Additive Mixed Model for mean daily thermal excess ( C), adjusted R 2 =50%.

Satellite-derived environmental drivers for top predator hotspots

Satellite-derived environmental drivers for top predator hotspots Satellite-derived environmental drivers for top predator hotspots Peter Miller @PeterM654 South West Marine Ecosystems 2017 21 Apr. 2017, Plymouth University Satellite environmental drivers for hotspots

More information

time window (mins)

time window (mins) Supplementary Material Gemma Carroll, Jason D. Everett, Robert Harcourt, David Slip, Ian Jonsen High sea surface temperatures driven by a strengthening current reduce foraging success by penguins cpue

More information

Comparison Figures from the New 22-Year Daily Eddy Dataset (January April 2015)

Comparison Figures from the New 22-Year Daily Eddy Dataset (January April 2015) Comparison Figures from the New 22-Year Daily Eddy Dataset (January 1993 - April 2015) The figures on the following pages were constructed from the new version of the eddy dataset that is available online

More information

Environmental forcing on forage fish and apex predators in the California Current: Results from a fully coupled ecosystem model

Environmental forcing on forage fish and apex predators in the California Current: Results from a fully coupled ecosystem model Environmental forcing on forage fish and apex predators in the California Current: Results from a fully coupled ecosystem model Jerome Fiechter Institute of Marine Sciences, UC Santa Cruz Co-authors: K.

More information

Spatial dynamics of small pelagic fish in the California Current system on the regime time-scale. Parallel processes in other species-ecosystems.

Spatial dynamics of small pelagic fish in the California Current system on the regime time-scale. Parallel processes in other species-ecosystems. PICES/GLOBEC Symposium Honolulu, Hawaii April 19-21, 2006 Spatial dynamics of small pelagic fish in the California Current system on the regime time-scale. Parallel processes in other species-ecosystems.

More information

Spatio-temporal dynamics of Marbled Murrelet hotspots during nesting in nearshore waters along the Washington to California coast

Spatio-temporal dynamics of Marbled Murrelet hotspots during nesting in nearshore waters along the Washington to California coast Western Washington University Western CEDAR Salish Sea Ecosystem Conference 2014 Salish Sea Ecosystem Conference (Seattle, Wash.) May 1st, 10:30 AM - 12:00 PM Spatio-temporal dynamics of Marbled Murrelet

More information

California 120 Day Precipitation Outlook Issued Tom Dunklee Global Climate Center

California 120 Day Precipitation Outlook Issued Tom Dunklee Global Climate Center California 120 Day Precipitation Outlook Issued 11-01-2008 Tom Dunklee Global Climate Center This is my second updated outlook for precipitation patterns and amounts for the next 4 s of the current rainy

More information

Genesis Parameters, Genesis Thresholds, and Mid-Level Humidity

Genesis Parameters, Genesis Thresholds, and Mid-Level Humidity Genesis Parameters, Genesis Thresholds, and Mid-Level Humidity Michael G. McGauley and David S. Nolan Rosenstiel School of Marine and Atmospheric Science University of Miami Miami, Florida, USA This work

More information

Supplementary Figure 1 Annual number of F0-F5 (grey) and F2-F5 (black) tornado observations over 30 years ( ) for Canada and United States.

Supplementary Figure 1 Annual number of F0-F5 (grey) and F2-F5 (black) tornado observations over 30 years ( ) for Canada and United States. SUPPLEMENTARY FIGURES Supplementary Figure 1 Annual number of F0-F5 (grey) and F2-F5 (black) tornado observations over 30 years (1980-2009) for Canada and United States. Supplementary Figure 2 Differences

More information

Principal Component Analysis of Sea Surface Temperature via Singular Value Decomposition

Principal Component Analysis of Sea Surface Temperature via Singular Value Decomposition Principal Component Analysis of Sea Surface Temperature via Singular Value Decomposition SYDE 312 Final Project Ziyad Mir, 20333385 Jennifer Blight, 20347163 Faculty of Engineering Department of Systems

More information

5th Meeting of the Scientific Committee Shanghai, China, September 2017

5th Meeting of the Scientific Committee Shanghai, China, September 2017 5th Meeting of the Scientific Committee Shanghai, China, 3-8 September 017 SC5-SQ06 Impacts of Climate variability on habitat suitability of Jumbo flying squid in the Southeast Pacific Ocean off Peruvian

More information

Northeast U.S. Early Season Preview 2017 FISHING ACTION STARTING TO WARM UP ALREADY WITH LOTS OF FISH EXPECTED IN MAY

Northeast U.S. Early Season Preview 2017 FISHING ACTION STARTING TO WARM UP ALREADY WITH LOTS OF FISH EXPECTED IN MAY Northeast U.S. Early Season Preview 2017 FISHING ACTION STARTING TO WARM UP ALREADY WITH LOTS OF FISH EXPECTED IN MAY By Matthew A. Upton and Mitchell A. Roffer ROFFS concludes its 2017 spring preview

More information

Cambridge International Examinations Cambridge International Advanced Subsidiary and Advanced Level

Cambridge International Examinations Cambridge International Advanced Subsidiary and Advanced Level Cambridge International Examinations Cambridge International Advanced Subsidiary and Advanced Level *2554656732* MARINE SCIENCE 9693/01 Paper 1 AS Structured Questions October/November 2017 1 hour 30 minutes

More information

Outline. Building Delphinid Habitat Models with Passive Acoustic Monitoring Data. Study Area. Species. HARP Data Analysis. Instrumentation 10/23/09

Outline. Building Delphinid Habitat Models with Passive Acoustic Monitoring Data. Study Area. Species. HARP Data Analysis. Instrumentation 10/23/09 Outline Building Delphinid Habitat Models with Passive Acoustic Monitoring Data Data Collection Model Challenges True absence vs. false absence Data sampling differences Temporal scale of datasets Case

More information

Coastal Ocean Circulation Experiment off Senegal (COCES)

Coastal Ocean Circulation Experiment off Senegal (COCES) DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Coastal Ocean Circulation Experiment off Senegal (COCES) Pierre-Marie Poulain Istituto Nazionale di Oceanografia e di Geofisica

More information

Distributional changes of west coast species and impacts of climate change on species and species groups

Distributional changes of west coast species and impacts of climate change on species and species groups Distributional changes of west coast species and impacts of climate change on species and species groups Elliott Hazen 1 Ole Shelton 2 Eric Ward 2 1 NOAA Southwest Fisheries Science Center 2 NOAA Northwest

More information

Red Sea - Dead Sea Water Conveyance Study Program Additional Studies

Red Sea - Dead Sea Water Conveyance Study Program Additional Studies Red Sea - Dead Sea Water Conveyance Study Program Additional Studies Red Sea Study Final Report Annex 1 Field and laboratory activities carried out during the study and their results July 213 TABLE OF

More information

Seasonal forecasting as a stepping stone to climate adaptation in marine fisheries and aquaculture

Seasonal forecasting as a stepping stone to climate adaptation in marine fisheries and aquaculture Seasonal forecasting as a stepping stone to climate adaptation in marine fisheries and aquaculture Alistair Hobday Paige Eveson Jason Hartog Claire Spillman Projected changes (e.g. distribution) 11 species

More information

SARSIM Model Output for the Distribution of Sardine in Canadian, US and Mexican Waters. Richard Parrish October 13, 2015

SARSIM Model Output for the Distribution of Sardine in Canadian, US and Mexican Waters. Richard Parrish October 13, 2015 SARSIM Model Output for the Distribution of Sardine in Canadian, US and Mexican Waters. Richard Parrish October 13, 2015 Agenda Item H.1.c The information presented below was taken from a model that I

More information

Multivariate time-series forecasting of the NE Arabian Sea Oil Sardine fishery using satellite covariates

Multivariate time-series forecasting of the NE Arabian Sea Oil Sardine fishery using satellite covariates Multivariate time-series forecasting of the NE Arabian Sea Oil Sardine fishery using satellite covariates Eli Holmes 1, Nimit Kumar 2, Sourav Maity 2, B.R Smitha 3, Sherine Cubelio 3, Cara Wilson 4, Narayanane

More information

Electronic Supplementary Material. Migration and Habitat of White Sharks (Carcharodon carcharias) in the Eastern Pacific Ocean.

Electronic Supplementary Material. Migration and Habitat of White Sharks (Carcharodon carcharias) in the Eastern Pacific Ocean. Electronic Supplementary Material Migration and Habitat of White Sharks (Carcharodon carcharias) in the Eastern Pacific Ocean Kevin C. Weng 1,2, Andre M. Boustany 1,3, Peter Pyle 4,5, Scot D. Anderson

More information

Glossary. The ISI glossary of statistical terms provides definitions in a number of different languages:

Glossary. The ISI glossary of statistical terms provides definitions in a number of different languages: Glossary The ISI glossary of statistical terms provides definitions in a number of different languages: http://isi.cbs.nl/glossary/index.htm Adjusted r 2 Adjusted R squared measures the proportion of the

More information

Identification of Large Pelagic Shark Habitats in the Central North Pacific Using PSATs, Satellite Remote Sensing, and SODA Assimilation Ocean Models

Identification of Large Pelagic Shark Habitats in the Central North Pacific Using PSATs, Satellite Remote Sensing, and SODA Assimilation Ocean Models Identification of Large Pelagic Shark Habitats in the Central North Pacific Using PSATs, Satellite Remote Sensing, and SODA Assimilation Ocean Models R. Michael Laurs 1, David G. Foley 2, and Michael Musyl

More information

R. Michael Laurs 1, David G. Foley 2, and Michael Musyl 2. RML Fisheries Oceanographer Consultant, LLC, Jacksonville, OR USA

R. Michael Laurs 1, David G. Foley 2, and Michael Musyl 2. RML Fisheries Oceanographer Consultant, LLC, Jacksonville, OR USA Update on Research Regarding Identification and Utilization Of Habitats by Large Pacific Sharks Using PSAT Archival Tags, Oceanic Satellite Remote Sensing, and SODA Ocean Assimilation Model Analyses R.

More information

LESSON THREE Time, Temperature, Chlorophyll a Does sea surface temperature affect chlorophyll a concentrations?

LESSON THREE Time, Temperature, Chlorophyll a Does sea surface temperature affect chlorophyll a concentrations? STUDENT PAGES LESSON THREE A partnership between California Current Ecosystem Long Term Ecological Research (CCE LTER) and Ocean Institute (OI) Beth Simmons, Education and Outreach Coordinator, CCE LTER,

More information

Salmon prey assemblages and oceanographic conditions along the California Current shelf ecosystem

Salmon prey assemblages and oceanographic conditions along the California Current shelf ecosystem Salmon prey assemblages and oceanographic conditions along the California Current shelf ecosystem Whitney Friedman, Brian Wells (presenting), John Field, Ric Brodeur, David Huff, Isaac Schroeder, Jarrod

More information

Species specific geographical distribution patterns in a warm Barents Sea: haddock vs. cod

Species specific geographical distribution patterns in a warm Barents Sea: haddock vs. cod Species specific geographical distribution patterns in a warm Barents Sea: haddock vs. cod Nordic Climate-Fish 2nd Conference: Latitudinal changes in marine resources, exploitation and society within the

More information

ANNUAL CLIMATE REPORT 2016 SRI LANKA

ANNUAL CLIMATE REPORT 2016 SRI LANKA ANNUAL CLIMATE REPORT 2016 SRI LANKA Foundation for Environment, Climate and Technology C/o Mahaweli Authority of Sri Lanka, Digana Village, Rajawella, Kandy, KY 20180, Sri Lanka Citation Lokuhetti, R.,

More information

2001 State of the Ocean: Chemical and Biological Oceanographic Conditions in the Newfoundland Region

2001 State of the Ocean: Chemical and Biological Oceanographic Conditions in the Newfoundland Region Stock Status Report G2-2 (2) 1 State of the Ocean: Chemical and Biological Oceanographic Conditions in the Background The Altantic Zone Monitoring Program (AZMP) was implemented in 1998 with the aim of

More information

CICESE Update. S. G. Marinone Edgar G. Pavia. January 2017

CICESE Update. S. G. Marinone Edgar G. Pavia. January 2017 CICESE Update S. G. Marinone Edgar G. Pavia SCCOOS BOG Meeting Ca San Pedro, January 217 Outline/Highlights 1. Transboundary fisheries and biological migrations 2. Marginal Sea and MPA (Gulf of California)

More information

Figure ES1 demonstrates that along the sledging

Figure ES1 demonstrates that along the sledging UPPLEMENT AN EXCEPTIONAL SUMMER DURING THE SOUTH POLE RACE OF 1911/12 Ryan L. Fogt, Megan E. Jones, Susan Solomon, Julie M. Jones, and Chad A. Goergens This document is a supplement to An Exceptional Summer

More information

Produced by Canadian Ice Service of. 2 December Seasonal Outlook Gulf of St Lawrence and East Newfoundland Waters Winter

Produced by Canadian Ice Service of. 2 December Seasonal Outlook Gulf of St Lawrence and East Newfoundland Waters Winter Environment Canada Environnement Canada Produced by Canadian Ice Service of Environment Canada 2 December 2010 Seasonal Outlook Gulf of St Lawrence and East Newfoundland Waters Winter 2010-2011 2010 Canadian

More information

Statistical Forecast of the 2001 Western Wildfire Season Using Principal Components Regression. Experimental Long-Lead Forecast Bulletin

Statistical Forecast of the 2001 Western Wildfire Season Using Principal Components Regression. Experimental Long-Lead Forecast Bulletin Statistical Forecast of the 2001 Western Wildfire Season Using Principal Components Regression contributed by Anthony L. Westerling 1, Daniel R. Cayan 1,2, Alexander Gershunov 1, Michael D. Dettinger 2

More information

Pacific Decadal Oscillation ( PDO ):

Pacific Decadal Oscillation ( PDO ): Time again for my annual Winter Weather Outlook. Here's just a small part of the items I considered this year and how I think they will play out with our winter of 2015-2016. El Nino / La Nina: When looking

More information

Which Earth latitude receives the greatest intensity of insolation when Earth is at the position shown in the diagram? A) 0 B) 23 N C) 55 N D) 90 N

Which Earth latitude receives the greatest intensity of insolation when Earth is at the position shown in the diagram? A) 0 B) 23 N C) 55 N D) 90 N 1. In which list are the forms of electromagnetic energy arranged in order from longest to shortest wavelengths? A) gamma rays, x-rays, ultraviolet rays, visible light B) radio waves, infrared rays, visible

More information

Climate Prediction Center National Centers for Environmental Prediction

Climate Prediction Center National Centers for Environmental Prediction NOAA s Climate Prediction Center Monthly and Seasonal Forecast Operations Wassila M. Thiaw Climate Prediction Center National Centers for Environmental Prediction Acknowlegement: Mathew Rosencrans, Arun

More information

Predicting summer pelagic habitat hotspots of neon flying squid (Ommastrephes bartramii) in the western North Pacific

Predicting summer pelagic habitat hotspots of neon flying squid (Ommastrephes bartramii) in the western North Pacific Predicting summer pelagic habitat hotspots of neon flying squid (Ommastrephes bartramii) in the western North Pacific Irene D. Alabia 1, Sei-Ichi Saitoh 1, Hiromichi Igarashi 2, Yoichi Ishikawa 2, Norihisa

More information

Name ECOLOGY TEST #1 Fall, 2014

Name ECOLOGY TEST #1 Fall, 2014 Name ECOLOGY TEST #1 Fall, 2014 Answer the following questions in the spaces provided. The value of each question is given in parentheses. Devote more explanation to questions of higher point value. 1.

More information

ENSO: Recent Evolution, Current Status and Predictions. Update prepared by: Climate Prediction Center / NCEP 9 November 2015

ENSO: Recent Evolution, Current Status and Predictions. Update prepared by: Climate Prediction Center / NCEP 9 November 2015 ENSO: Recent Evolution, Current Status and Predictions Update prepared by: Climate Prediction Center / NCEP 9 November 2015 Outline Summary Recent Evolution and Current Conditions Oceanic Niño Index (ONI)

More information

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 5 August 2013

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 5 August 2013 ENSO Cycle: Recent Evolution, Current Status and Predictions Update prepared by Climate Prediction Center / NCEP 5 August 2013 Outline Overview Recent Evolution and Current Conditions Oceanic Niño Index

More information

Climate Outlook and Review

Climate Outlook and Review Climate Outlook and Review September 2018 Author: Prof Roger C Stone Overview The European, UK, and US long-term climate models that focus on forecasting central Pacific sea surface temperatures are continuing

More information

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 23 April 2012

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 23 April 2012 ENSO Cycle: Recent Evolution, Current Status and Predictions Update prepared by Climate Prediction Center / NCEP 23 April 2012 Outline Overview Recent Evolution and Current Conditions Oceanic Niño Index

More information

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 11 November 2013

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 11 November 2013 ENSO Cycle: Recent Evolution, Current Status and Predictions Update prepared by Climate Prediction Center / NCEP 11 November 2013 Outline Overview Recent Evolution and Current Conditions Oceanic Niño Index

More information

PICES W3 [D-504], Sep 22, 2017, 11:40-12:05

PICES W3 [D-504], Sep 22, 2017, 11:40-12:05 PICES W3 [D-504], Sep 22, 2017, 11:40-12:05 Individual-based model of chub mackerel (Scomber japonicus) covering from larval to adult stages to project climate-driven changes in their spatial distribution

More information

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 25 February 2013

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 25 February 2013 ENSO Cycle: Recent Evolution, Current Status and Predictions Update prepared by Climate Prediction Center / NCEP 25 February 2013 Outline Overview Recent Evolution and Current Conditions Oceanic Niño Index

More information

Serial No. N4470 NAFO SCR Doc. 01/83 SCIENTIFIC COUNCIL MEETING SEPTEMBER 2001

Serial No. N4470 NAFO SCR Doc. 01/83 SCIENTIFIC COUNCIL MEETING SEPTEMBER 2001 NOT TO BE CITED WITHOUT PRIOR REFERENCE TO THE AUTHOR(S) Northwest Atlantic Fisheries Organization Serial No. N7 NAFO SCR Doc. /8 SCIENTIFIC COUNCIL MEETING SEPTEMBER Sea-surface Temperature and Water

More information

Persistence of prey hot spots in southeast Alaska

Persistence of prey hot spots in southeast Alaska Persistence of prey hot spots in southeast Alaska Scott M. Gende National Park Service, Glacier Bay Field Station, 3100 National Park, Juneau, Alaska, USA; Scott_Gende Gende@nps.gov Michael Sigler National

More information

ENSO: Recent Evolution, Current Status and Predictions. Update prepared by: Climate Prediction Center / NCEP 30 October 2017

ENSO: Recent Evolution, Current Status and Predictions. Update prepared by: Climate Prediction Center / NCEP 30 October 2017 ENSO: Recent Evolution, Current Status and Predictions Update prepared by: Climate Prediction Center / NCEP 30 October 2017 Outline Summary Recent Evolution and Current Conditions Oceanic Niño Index (ONI)

More information

Climate Outlook and Review

Climate Outlook and Review Climate Outlook and Review August 2018 Author: Prof Roger C Stone Overview The European, UK, and US long-term climate models that focus on forecasting central Pacific sea surface temperatures are continuing

More information

4.3.2 Configuration. 4.3 Ensemble Prediction System Introduction

4.3.2 Configuration. 4.3 Ensemble Prediction System Introduction 4.3 Ensemble Prediction System 4.3.1 Introduction JMA launched its operational ensemble prediction systems (EPSs) for one-month forecasting, one-week forecasting, and seasonal forecasting in March of 1996,

More information

El Nino: Outlook VAM-WFP HQ September 2018

El Nino: Outlook VAM-WFP HQ September 2018 El Nino: Outlook 2018 VAM-WFP HQ September 2018 El Nino Outlook September 2018 2015-16 El Nino Peak Possible evolution of an El Nino indicator (Pacific sea surface temperature anomaly) generated by a diverse

More information

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 24 September 2012

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 24 September 2012 ENSO Cycle: Recent Evolution, Current Status and Predictions Update prepared by Climate Prediction Center / NCEP 24 September 2012 Outline Overview Recent Evolution and Current Conditions Oceanic Niño

More information

Meteorology. Circle the letter that corresponds to the correct answer

Meteorology. Circle the letter that corresponds to the correct answer Chapter 3 Worksheet 1 Meteorology Name: Circle the letter that corresponds to the correct answer 1) If the maximum temperature for a particular day is 26 C and the minimum temperature is 14 C, the daily

More information

Seasonal Climate Watch July to November 2018

Seasonal Climate Watch July to November 2018 Seasonal Climate Watch July to November 2018 Date issued: Jun 25, 2018 1. Overview The El Niño-Southern Oscillation (ENSO) is now in a neutral phase and is expected to rise towards an El Niño phase through

More information

Fire Weather Drivers, Seasonal Outlook and Climate Change. Steven McGibbony, Severe Weather Manager Victoria Region Friday 9 October 2015

Fire Weather Drivers, Seasonal Outlook and Climate Change. Steven McGibbony, Severe Weather Manager Victoria Region Friday 9 October 2015 Fire Weather Drivers, Seasonal Outlook and Climate Change Steven McGibbony, Severe Weather Manager Victoria Region Friday 9 October 2015 Outline Weather and Fire Risk Environmental conditions leading to

More information

Hiromichi Igarashi 1,2, Y. Ishikawa 1, T. Wakamatsu 1, Y. Tanaka 1, M. Kamachi 1,3, N. Usui 3, M. Sakai 4, S. Saitoh 2 and Y.

Hiromichi Igarashi 1,2, Y. Ishikawa 1, T. Wakamatsu 1, Y. Tanaka 1, M. Kamachi 1,3, N. Usui 3, M. Sakai 4, S. Saitoh 2 and Y. PICES2015,Qingdao Oct.20,2015 Relationships between ocean conditions and interannual variability of habitat suitability index (HSI) distribution for neon flying squid in central North Pacific examined

More information

Hydrography and biological resources in the western Bering Sea. Gennady V. Khen, Eugeny O. Basyuk. Pacific Research Fisheries Centre (TINRO-Centre)

Hydrography and biological resources in the western Bering Sea. Gennady V. Khen, Eugeny O. Basyuk. Pacific Research Fisheries Centre (TINRO-Centre) Hydrography and biological resources in the western Bering Sea Gennady V. Khen, Eugeny O. Basyuk Pacific Research Fisheries Centre (TINRO-Centre) Bering Sea: deep-sea basin, shelf, and US-Russia convention

More information

Coastal Ocean Circulation Experiment off Senegal (COCES)

Coastal Ocean Circulation Experiment off Senegal (COCES) DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Coastal Ocean Circulation Experiment off Senegal (COCES) Pierre-Marie Poulain Istituto Nazionale di Oceanografia e di Geofisica

More information

Supplementary Figure 1 Surface distribution and concentration of the dinoflagellate N. scintillans

Supplementary Figure 1 Surface distribution and concentration of the dinoflagellate N. scintillans Supplementary Figure 1: Surface distribution and concentration of the dinoflagellate N. scintillans (cells l-1) in the Arabian Sea during the winter monsoons of 2000-2011 (1-100 cells l-1, 8000-10,000

More information

Climate Outlook and Review Focus on sugar industry requirements. Issued 1 October Roger C Stone

Climate Outlook and Review Focus on sugar industry requirements. Issued 1 October Roger C Stone Climate Outlook and Review Focus on sugar industry requirements Issued 1 October 2017 Roger C Stone University of Southern Queensland Document title 1 Overview A short La Nina-type pattern trying to develop

More information

RESEARCH REPORT SERIES

RESEARCH REPORT SERIES GREAT AUSTRALIAN BIGHT RESEARCH PROGRAM RESEARCH REPORT SERIES Regional Availability of MODIS Imagery in the Great Australian Bight Ana Redondo Rodriguez1 Edward King2 and Mark Doubell1 SARDI Aquatic Sciences

More information

New Zealand Climate Update No 226, April 2018 Current climate March 2018

New Zealand Climate Update No 226, April 2018 Current climate March 2018 New Zealand Climate Update No 226, April 2018 Current climate March 2018 March 2018 was characterised by significantly higher pressure than normal to the east of New Zealand. This pressure pattern, in

More information

SCW6-Doc05. CPUE standardization for the offshore fleet fishing for Jack mackerel in the SPRFMO area

SCW6-Doc05. CPUE standardization for the offshore fleet fishing for Jack mackerel in the SPRFMO area 6th Scientific Committee Workshop Valparaiso, Chile 28-30 May 2018 SCW6-Doc05 CPUE standardization for the offshore fleet fishing for Jack mackerel in the SPRFMO area M.A. Pastoors & N.T. Hintzen (European

More information

Trends in policing effort and the number of confiscations for West Coast rock lobster

Trends in policing effort and the number of confiscations for West Coast rock lobster Trends in policing effort and the number of confiscations for West Coast rock lobster A. Brandão, S. Johnston and D.S. Butterworth Marine Resource Assessment & Management Group (MARAM) Department of Mathematics

More information

Winter. Here s what a weak La Nina usually brings to the nation with tempseraures:

Winter. Here s what a weak La Nina usually brings to the nation with tempseraures: 2017-2018 Winter Time again for my annual Winter Weather Outlook. Here's just a small part of the items I considered this year and how I think they will play out with our winter of 2017-2018. El Nino /

More information

Preparation and dissemination of the averaged maps and fields of selected satellite parameters for the Black Sea within the SeaDataNet project

Preparation and dissemination of the averaged maps and fields of selected satellite parameters for the Black Sea within the SeaDataNet project Journal of Environmental Protection and Ecology 11, No 4, 1568 1578 (2010) Environmental informatics Preparation and dissemination of the averaged maps and fields of selected satellite parameters for the

More information

UPDATE OF REGIONAL WEATHER AND SMOKE HAZE (February 2018)

UPDATE OF REGIONAL WEATHER AND SMOKE HAZE (February 2018) UPDATE OF REGIONAL WEATHER AND SMOKE HAZE (February 2018) 1. Review of Regional Weather Conditions for January 2018 1.1 The prevailing Northeast monsoon conditions over Southeast Asia strengthened in January

More information

The U. S. Winter Outlook

The U. S. Winter Outlook The 2017-2018 U. S. Winter Outlook Michael Halpert Deputy Director Climate Prediction Center Mike.Halpert@noaa.gov http://www.cpc.ncep.noaa.gov Outline About the Seasonal Outlook Review of 2016-17 U. S.

More information

Jeffrey Polovina 1, John Dunne 2, Phoebe Woodworth 1, and Evan Howell 1

Jeffrey Polovina 1, John Dunne 2, Phoebe Woodworth 1, and Evan Howell 1 Projected expansion of the subtropical biome and contraction of the temperate and equatorial upwelling biomes in the North Pacific under global warming Jeffrey Polovina 1, John Dunne 2, Phoebe Woodworth

More information

Seasonal Climate Watch January to May 2016

Seasonal Climate Watch January to May 2016 Seasonal Climate Watch January to May 2016 Date: Dec 17, 2015 1. Advisory Most models are showing the continuation of a strong El-Niño episode towards the latesummer season with the expectation to start

More information

Sudan Seasonal Monitor

Sudan Seasonal Monitor Sudan Seasonal Monitor Sudan Meteorological Authority Federal Ministry of Agriculture and Forestry Issue 5 August 2010 Summary Advanced position of ITCZ during July to most north of Sudan emerged wide

More information

Movements of striped bass in response to extreme weather events

Movements of striped bass in response to extreme weather events Movements of striped bass in response to extreme weather events Helen Bailey and David Secor E-mail: hbailey@umces.edu 1 Background 2 Outline What is movement ecology? Methods for analyzing animal tracks

More information

on climate and its links with Arctic sea ice cover

on climate and its links with Arctic sea ice cover The influence of autumnal Eurasian snow cover on climate and its links with Arctic sea ice cover Guillaume Gastineau* 1, Javier García- Serrano 2 and Claude Frankignoul 1 1 Sorbonne Universités, UPMC/CNRS/IRD/MNHN,

More information

J.P. Glazer and D.S. Butterworth

J.P. Glazer and D.S. Butterworth A summary of the General Linear Modelling approach applied to standardize the CPUE data for the offshore trawl fishery for Merluccius capensis and M. paradoxus off the coast of South Africa. Introduction

More information

Will a warmer world change Queensland s rainfall?

Will a warmer world change Queensland s rainfall? Will a warmer world change Queensland s rainfall? Nicholas P. Klingaman National Centre for Atmospheric Science-Climate Walker Institute for Climate System Research University of Reading The Walker-QCCCE

More information

Seasonal Climate Watch September 2018 to January 2019

Seasonal Climate Watch September 2018 to January 2019 Seasonal Climate Watch September 2018 to January 2019 Date issued: Aug 31, 2018 1. Overview The El Niño-Southern Oscillation (ENSO) is still in a neutral phase and is still expected to rise towards an

More information

Here s what a weak El Nino usually brings to the nation with temperatures:

Here s what a weak El Nino usually brings to the nation with temperatures: Time again for my annual Winter Weather Outlook. Here's just a small part of the items I considered this year and how I think they will play out with our winter of 2018-2019. El Nino / La Nina: When looking

More information

Practice Seasons Moon Quiz

Practice Seasons Moon Quiz 1. Which diagram represents the tilt of Earth's axis relative to the Sun's rays on December 15? A) B) C) D) 2. The diagram below represents Earth in space on the first day of a season. 5. Base your answer

More information

Chapter 3. Regression-Based Models for Developing Commercial Demand Characteristics Investigation

Chapter 3. Regression-Based Models for Developing Commercial Demand Characteristics Investigation Chapter Regression-Based Models for Developing Commercial Demand Characteristics Investigation. Introduction Commercial area is another important area in terms of consume high electric energy in Japan.

More information

Determine the trend for time series data

Determine the trend for time series data Extra Online Questions Determine the trend for time series data Covers AS 90641 (Statistics and Modelling 3.1) Scholarship Statistics and Modelling Chapter 1 Essent ial exam notes Time series 1. The value

More information

Multivariate Regression Model Results

Multivariate Regression Model Results Updated: August, 0 Page of Multivariate Regression Model Results 4 5 6 7 8 This exhibit provides the results of the load model forecast discussed in Schedule. Included is the forecast of short term system

More information

Bugs in JRA-55 snow depth analysis

Bugs in JRA-55 snow depth analysis 14 December 2015 Climate Prediction Division, Japan Meteorological Agency Bugs in JRA-55 snow depth analysis Bugs were recently found in the snow depth analysis (i.e., the snow depth data generation process)

More information

Seasonal Climate Watch June to October 2018

Seasonal Climate Watch June to October 2018 Seasonal Climate Watch June to October 2018 Date issued: May 28, 2018 1. Overview The El Niño-Southern Oscillation (ENSO) has now moved into the neutral phase and is expected to rise towards an El Niño

More information

Decadal changes in sea surface temperature, wave forces and intertidal structure in New Zealand

Decadal changes in sea surface temperature, wave forces and intertidal structure in New Zealand The following supplement accompanies the article Decadal changes in sea surface temperature, wave forces and intertidal structure in New Zealand David R. Schiel*, Stacie A. Lilley, Paul M. South, Jack

More information

NOAA 2015 Updated Atlantic Hurricane Season Outlook

NOAA 2015 Updated Atlantic Hurricane Season Outlook NOAA 2015 Updated Atlantic Hurricane Season Outlook Dr. Gerry Bell Lead Seasonal Forecaster Climate Prediction Center/ NOAA/ NWS Collaboration With National Hurricane Center/ NOAA/ NWS Hurricane Research

More information

Phytoplankton. Zooplankton. Nutrients

Phytoplankton. Zooplankton. Nutrients Phytoplankton Zooplankton Nutrients Patterns of Productivity There is a large Spring Bloom in the North Atlantic (temperate latitudes remember the Gulf Stream!) What is a bloom? Analogy to terrestrial

More information

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 15 July 2013

ENSO Cycle: Recent Evolution, Current Status and Predictions. Update prepared by Climate Prediction Center / NCEP 15 July 2013 ENSO Cycle: Recent Evolution, Current Status and Predictions Update prepared by Climate Prediction Center / NCEP 15 July 2013 Outline Overview Recent Evolution and Current Conditions Oceanic Niño Index

More information

The increasing intensity of the strongest tropical cyclones

The increasing intensity of the strongest tropical cyclones The increasing intensity of the strongest tropical cyclones James B. Elsner Department of Geography, Florida State University Tallahassee, Florida Corresponding author address: Dept. of Geography, The

More information

C) the seasonal changes in constellations viewed in the night sky D) The duration of insolation will increase and the temperature will increase.

C) the seasonal changes in constellations viewed in the night sky D) The duration of insolation will increase and the temperature will increase. 1. Which event is a direct result of Earth's revolution? A) the apparent deflection of winds B) the changing of the Moon phases C) the seasonal changes in constellations viewed in the night sky D) the

More information

The observed global warming of the lower atmosphere

The observed global warming of the lower atmosphere WATER AND CLIMATE CHANGE: CHANGES IN THE WATER CYCLE 3.1 3.1.6 Variability of European precipitation within industrial time CHRISTIAN-D. SCHÖNWIESE, SILKE TRÖMEL & REINHARD JANOSCHITZ SUMMARY: Precipitation

More information

The seasonal and interannual variability of circulation in the eastern and western Okhotsk Sea and its impact on plankton biomass

The seasonal and interannual variability of circulation in the eastern and western Okhotsk Sea and its impact on plankton biomass The seasonal and interannual variability of circulation in the eastern and western Okhotsk Sea and its impact on plankton biomass Andrey G. Andreev, Sergey V. Prants, Maxim V. Budyansky and Michael Yu.

More information

53 contributors for 35 individual reports in 2009 show 5% of figures today

53 contributors for 35 individual reports in 2009 show 5% of figures today A Group Approach to Understanding Ecosystem Dynamics in the Northeast Pacific Ocean William Crawford and James Irvine, Fisheries and Oceans Canada (DFO) * * * 53 contributors for 35 individual reports

More information

Southern Florida to Cape Hatteras Early Season Preview 2017 U.S. EAST COAST GULF STREAM CONDITIONS LOOKING PROMISING

Southern Florida to Cape Hatteras Early Season Preview 2017 U.S. EAST COAST GULF STREAM CONDITIONS LOOKING PROMISING Southern Florida to Cape Hatteras Early Season Preview 2017 U.S. EAST COAST GULF STREAM CONDITIONS LOOKING PROMISING By Matthew A. Upton and Mitchell A. Roffer ROFFS continues its spring preview series

More information

ONE-YEAR EXPERIMENT IN NUMERICAL PREDICTION OF MONTHLY MEAN TEMPERATURE IN THE ATMOSPHERE-OCEAN-CONTINENT SYSTEM

ONE-YEAR EXPERIMENT IN NUMERICAL PREDICTION OF MONTHLY MEAN TEMPERATURE IN THE ATMOSPHERE-OCEAN-CONTINENT SYSTEM 71 4 MONTHLY WEATHER REVIEW Vol. 96, No. 10 ONE-YEAR EXPERIMENT IN NUMERICAL PREDICTION OF MONTHLY MEAN TEMPERATURE IN THE ATMOSPHERE-OCEAN-CONTINENT SYSTEM JULIAN ADEM and WARREN J. JACOB Extended Forecast

More information

Oct.23,2014. PICES2014,Yeosu

Oct.23,2014. PICES2014,Yeosu PICES2014,Yeosu Oct.23,2014 A multi-model ensemble prediction of habitat suitability index (HSI) models for neon flying squid in central North Pacific by using 3-D ocean data assimilation product Hiromichi

More information

Non-breeding distribution and activity patterns in a temperate population of brown skua

Non-breeding distribution and activity patterns in a temperate population of brown skua The following supplement accompanies the article Non-breeding distribution and activity patterns in a temperate population of brown skua Hendrik Schultz, Rebecca J. Hohnhold, Graeme A. Taylor, Sarah J.

More information

Solar photovoltaic energy production comparison of east, west, south-facing and tracked arrays

Solar photovoltaic energy production comparison of east, west, south-facing and tracked arrays The Canadian Society for Bioengineering The Canadian society for engineering in agricultural, food, environmental, and biological systems. La Société Canadienne de Génie Agroalimentaire et de Bioingénierie

More information

Malawi. General Climate. UNDP Climate Change Country Profiles. C. McSweeney 1, M. New 1,2 and G. Lizcano 1

Malawi. General Climate. UNDP Climate Change Country Profiles. C. McSweeney 1, M. New 1,2 and G. Lizcano 1 UNDP Climate Change Country Profiles Malawi C. McSweeney 1, M. New 1,2 and G. Lizcano 1 1. School of Geography and Environment, University of Oxford. 2. Tyndall Centre for Climate Change Research http://country-profiles.geog.ox.ac.uk

More information

North Pacific Climate Overview N. Bond (UW/JISAO), J. Overland (NOAA/PMEL) Contact: Last updated: September 2008

North Pacific Climate Overview N. Bond (UW/JISAO), J. Overland (NOAA/PMEL) Contact: Last updated: September 2008 North Pacific Climate Overview N. Bond (UW/JISAO), J. Overland (NOAA/PMEL) Contact: Nicholas.Bond@noaa.gov Last updated: September 2008 Summary. The North Pacific atmosphere-ocean system from fall 2007

More information

Characteristics of Storm Tracks in JMA s Seasonal Forecast Model

Characteristics of Storm Tracks in JMA s Seasonal Forecast Model Characteristics of Storm Tracks in JMA s Seasonal Forecast Model Akihiko Shimpo 1 1 Climate Prediction Division, Japan Meteorological Agency, Japan Correspondence: ashimpo@naps.kishou.go.jp INTRODUCTION

More information