Catch dynamics of small pelagic fishes at Bali Strait & South Java Sea ...

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Mar 11, 2017 - 14-year monthly Catch per Unit Effort (CpUE) of SPF catch data provided by Muncar. Fishing Port (Bali Strait) and South Java. • 14-year ...
INTERNATIONAL SYMPOSIUM DRIVERS OF DYNAMICS OF SMALL PELAGIC FISH RESOURCES MARCH 6-11, 2017 VICTORIA, CANADA

Catch dynamics of small pelagic fishes at Bali Strait & South Java Sea in relation to the climatic regime shift: case study on Sardinella lemuru Aida Sartimbul, Erfan Rohadi, Defri Yona, Hideaki Nakata, Jogi Arleston, Iwan T Wibowo, Kirana F Setiabudi, Kharisma W Sesanti Marine Science Resources Exploration and Management Research Group Marine Science Dept. of Brawijaya University, Malang, Indonesia Information Management, State Polytechnic of Malang, Indonesia Fisheries Faculty, Nagasaki University, Japan

Outline: • • • • • • • • •

Introduction Objective Data and Methods Result and Discussion Small Pelagic Fish CPUE Trend Seasonal Variation Inter-annual Variation Regime Shift Summary

Background S. Lemuru (SPF) main species target of Bali Strait (80-90%), followed by Decapterus spp. and Euthynus spp. (Merta et al., 1995; Hendiarti et al, 2005) S. Lemuru  supporting public health ( >25% of total sardine oil were contained omega-3 fatty acid) (Sartimbul et al., 2015) It was disappeared in 2010 to 2012 it gave impact on economics loss mainly for coastal community Limited study related to the SPF dynamics and its relation to the climate change and regime shift in Indonesia……….

Objectives Understanding the variability of SPF catch Understanding the SPF catch composition and its relation to the oceanographic features Understanding the SPF catch variability in relation to the regime shift and climate variability

Introduction

Material and Methods

Result and Discussion

Conclusion

1st Station : 1140 26’ 11” BT 08 27’ 14” LS 2nd Station : 1140 34’ 43” BT 08 37’ 08” LS 3rd Station : 1140 40’16 BT 08 42’ 18” LS (Fishing Ground at Bali Strait

Study Area

Temperature and Clorophyl-a Insitu Data : June – December 2013 Temperature and Clorophyl-a Satellite Data : February 2002 - April 2015 Introduction

Material and Methods

Result and Discussion

Conclusion

Sampling site of South Java (Fishing ground of S. lemuru)

• 14-year monthly Catch per Unit Effort (CpUE) of SPF catch data provided by Muncar Fishing Port (Bali Strait) and South Java • 14-year monthly satellite Aqua MODIS data of SST & Chl-a (2002-2015) (www.modis.gsfc.nasa.gov). • Monthly temp. and Chl-a Insitu Data were collected using AAQ Alec Japan (Jun – Dec 2013) • Plankton data were sampled on June-Dec, 2013 • Anomalies, standardization, statistics, and Regime shift detection (Rodionov, 2005) methods were applied in this study • Nino 3.4 and IOD were used as Climate index (NOAA, 2007)

Data and Methods

Insitu and Satellite Temperature Data Verification

No.

Model 1

R

R Square a

,945

,894

Adjusted R Square ,872

Date of Data Retrieval

Insitu Data

1

June 15, 2013

(0C) 30,00

2

July 20, 2013

3

Satellite Data (0C)

difference

29,34

(0C) 0,66

29,40

28,72

0,68

August 20, 2013

29,10

28,22

0,88

4

September 21, 2013

28,90

27,94

0,96

5

October 16, 2013

29,00

28,41

0,59

6

November 12, 2013

29,30

28,75

0,55

7

December 11, 2013

30,00

30,02

-0,02

Maximum Value

30,02

Minimum Value

27,94

Std. Error of the Estimate ,25324

Temp.

RESULT & DISCUSSION

Clorophyl-a Data Verification Date of

No.

Model

R

1

,951a

R Square

Adjusted R Square

,904

,885

Retrieval Data

Insitu

Satellite

Chl-a

Data

Data

difference

(mg/m3) 0,18

(mg/m3) -0,01

1

Jun 15, 2013

(mg/m3) 0,17

2

Jul 20, 2013

1,38

1,41

-0,04

3

Aug 20, 2013

2,04

2,22

-0,18

4

Sep 21, 2013

2,13

1,98

0,14*

5

Nov 16, 2013

1,14

1,26

-0,12

6

Nov 12, 2013

0,70

1,05

-0,36

7

Dec 11, 2013

0,64

0,38

0,26*

Maximum Value

2,13

Minimum Value

0,17

Std. Error of the Estimate ,24738

a. Predictors: (Constant), suhusatelitMODIS

Introduction

Material and Methods

Result and Discussion

Conclusion

Fish Catch landed in Bali Strait

Total Catch (Ton)

• Total Fish Catch in Bali Strait 70,000 60,000 50,000 40,000 30,000 20,000 10,000 0

Total Catch

2002 2003 2004 2005 2006 2007 2008 2009 2010 2011 2012 2013 2014 2015

Persentage (%)

Sardinella lemuru 100% 90% 80% 70% 60% 50% 40% 30% 20% 10%

2002

Decapterus spp

2003

2004

2005

2006

Euthynnus spp

2007

2008

2009

• Percentage Fish Dominant Landed in Bali Strait

2010

Other Fish

2011

2012

2013

2014

2015

6000.00

Transition I

5000.00

4191.00 4000.00 4163.64 3000.00 2000.00 1000.00 0.00

SE Monsoon

3956.67 3104.78 2994.42

3085.68 2937.28 2507.86 2214.97 NW 1803.20 Monso on J

F

Seasonal variation

6086.50 5411.99

M

A

M

J

J

Transition II

A

S

O

N

D

SST

• Max. catches of S. lemuru occurs in Trans-1 Monsoon • It is 3-month after upwelling event during SE monsoon (Sartimbul et al., 2010) • Intensive upwelling  the primarily production increases (Chl-a)

SST (DEG.C)

MONTH

31.00 30.0930.15 30.00 29.64 29.44 29.38 SE Monsoon 29.00 28.53 28.47 28.00 NW 27.24 27.08 27.00 Transition I 26.48 Monso 26.00 26.03 25.77 on 25.00 Transition II 24.00 23.00 J F M A M J J A S O N D MONTH

CHL-A (MG/M3)

CPUE S. LEMURU (KG)

S.lemuru

7000.00

1.60 1.40 1.20 1.00 0.80 0.60 0.40 0.20 0.00

Chl-a Transition I

0.27 0.32 0.23 F

1.21 1.19

1.02

NW Monso on

J

1.47

M

0.83 SE Monsoon

0.50

A

1.09 1.08

M

J

J

MONTH

A

Transition II

S

O

N

0.50

D

Inter-annual SPF Catch Composition and Oceanographic variation (a)

SST

(b)

Chl-a

(c)

(d)

(e)

Inter-annual catch variation

Gambar 32. Trend Anomali Bulanan Suhu (a), Klorofil (b) dan Ikan Dominan yang Tertangkap (c - e) di Perairan Selat Bali

3

SST

2 1 0 -1 -2 3 2

2002 2003 2004 2005 2006 2007 2008 2009 2010 2011 2012 2013 2014 2015

Chl-a

1 0 -1 -2 3

1

2

3

4

5

6

7

8

9

10

11

12

13

14

Nino 3.4

2 1 0 -1

1

2

3

4

5

6

7

8

9

10

11

12

13

14

-2 3 2 1 0 -1 1 2 3 4 3 2 Decapterus spp 1 0 -1 -2 1 2 3 4 2 1

5

5

6

6

7

7

8

8

9

9

10

10

11

11

12

12

13

Warming year (La Nina 2010) lowest fish catch in Bali Strait

13

14

14

Euthynnus spp

0 -1 -2

Cooling year (El Nino 2006)  peak fish catch of S. lemuru in Bali Strait

El Nino 2015 No consistency ???

S. lemuru

-2

Standardization parameters

2002 2003 2004 2005 2006 2007 2008 2009 2010 2011 2012 2013 2014 2015

Why???

But…..

EL Nino 2006 DAN 2015 (Nasa, 2016)

Regime Shift on S.lemuru S.lemuru

RSI

STARS

Ano CPUE Lemuru

Warm

10000

0.5 0

0

Cool

-10000

-0.5

-20000 2002 2003 2004 2005 2006 2007 2008 2009 2010 2011 2012 2013 2014 2015 Tahun SST

RSI

-1

STARS

1

0.5

Warm

0.5

1 RS

0.25

0

0

-0.5 -1 2002

Regime Shift Index

1

20000

-0.25

Cool 2003

2004

2005

2006

2007

2008

2009

2010

2011

2012

2013

2014

2015

-0.5

RS detection (Rodinov, 2005): based on sequential T-test for RS (Sequential T-test Analysis of RS/ STAR)

NINO 3.4

RSI

STARS

0.25

Nino 3.4

1.5

0

0

-0.25

-1.5

-3 2002

Regime Shift Index

0.5

3

2003

2004

2005

2006

2007

2008

2009

2010

2011

2012

2013

2014

2015

-0.5

Tahun DMI

RSI

STARS

0.5

0.25

0

0

-0.5

-1 2002

1 RS

0.5

Regime Shift Index

Dipole Mode Index

1

-0.25

2003

2004

2005

2006

2007

2008

2009 Tahun

2010

2011

2012

2013

2014

2015

-0.5

Sartimbul et al., 2010: Cool year and peak season of S.lemuru after 3-month moving average

Case study BPF at South Java

EL-NINO 2006-2007/ Cool year 900000

0

FISH CATCH (KG)

800000

-0.2

700000 600000

-0.4

500000 -0.6

400000 300000

-0.8

200000

-1

100000 0

Jan Feb Mar Apr Mei Jun

Jul Agu Sep Okt Nov Des

Cakalang

Tongkol

Tuna

Baby Tuna

Suhu Permukaan Laut

-1.2

SUHU PERMUKAAN LAUT (0C)

0.2

1000000

1,000,000

1.8

900,000

1.6

FISH CATCH (KG)

800,000

1.4

700,000

1.2

600,000

1

500,000

0.8

400,000

0.6

300,000

0.4

200,000

0.2

100,000 0

Jan Feb Mar Apr Mei Jun Jul Agu Sep Okt Nov Des Cakalang

Tongkol

Tuna

Baby Tuna

Suhu Permukaan Laut

0

SEA SURFACE TEMPERATURE (0C)

La-Nina 2010-2011/ Warm year

Thermocline Variation

Some possible reason of S.lemuru dynamics at Bali Strait and South Java Sea….. 1. Three-months time lagged for S.lemuru Modified from Sartimbul et al., (2010): Progress in Oceanography (87), 168-174 M a n a g e m e n t 2. Regime shift of S.lemuru  cool and warm period 3. Horizontal movement  further north or south 4. Vertical migration  deeper/shallower thermocline (La Nina/ El Nino)

Summary

1

• SPF composition were vary seasonally. • S.Lemuru (Trans-2), Decapterus spp (NW Monsoon), and Euthynnus spp (always appear in all seasons)

2

• 14-year fishing trends regime shift from seasonal to inter-annual variation • Change in fish composition from seasonal to interannual

3

• Cold year (ENSO and pIOD) in 2006-2007 S.lemuru reached peak catch • Warm year (La Nina) in 2010 – 2012, S.lemuru was lowest catch • El Nino 2015  low CPUE of S. lemuru may be caused by behavior of warmer El Nino

Introduction

Material and Methods

Result and Discussion

Conclusion

Future Task

1

• S.lemuru is important as key species of BPF lack of juvenile data

2

• Needed to develop new fishing ground map based on time lag and thermocline information

3

• Needed new climate index for Indonesia ocean system • Collaborations are welcome!

Introduction

Material and Methods

Result and Discussion

Conclusion

Thank you for your attention and contribution •

Ministry of Research, Technology and Higher Education of Indonesia • Brawijaya University • PICES

ACKNOWLEDGEMENT