Inductive reasoning and prediction of population dynamics of Cylindrospermopsis in the Wivenhoe Reservoir by means of evolutionary computation

Similar documents
In Vivo Monitoring of Blue-Green Algae Using Hydrolab Multi- Parameter Sondes

Main cyanobacterial genera that produce cyanotoxins: Dolichospermum sp. Source: Public Health Authority of the Slovak Republic

Ecology 3/15/2017. Today. Autotrophs. Writing Assignment: What does it mean. Last readings on Chlamydomonas populations

Homework 1 solutions

EC 331: Research in Applied Economics

AP Biology. Sample Student Responses and Scoring Commentary. Inside: Free Response Question 5. Scoring Guideline. Student Samples. Scoring Commentary

The only contamination levels for microbial contaminants in recreational and source waters are coliforms and the fecal bacteria E.

Vancouver Lake Biotic Assessment

Toxic Algae and Cyanobacteria in Recreational Waters. Rang Cho Miriam Moritz

Ensemble Data Assimilation of Water Quality Variables

Biophysical Interactions

Michelle Chaput Department of Geography, Environment and Geomatics University of Ottawa

Reclamation Perspective on Operational Snow Data and Needs. Snowpack Monitoring for Streamflow Forecasting and Drought Planning August 11, 2015

The horizontal heterogeneity of nitrogen fixation in Lake Valencia, Venezuela

Field Identification of Algae

Flood intelligence an international collaborative case study. Karin Geraghty, CIO, DEWNR

Applied Modeling & Forecasting. Chapter 1

Abstract. 1. Introduction

Amanda Murby University of New Hampshire. Cyanobacteria Monitoring and Analysis Workshop June 26, Cyanobacteria. Importance of Toxins and Size

Applied Modeling & Forecasting QMIS 320 Chapter 1

USA National Weather Service Community Hydrologic Prediction System

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

CopernicusEU. the EU's Earth Observation Programme. Sara Zennaro Atre Delegation of the European Union to Japan

Defining Normal Weather for Energy and Peak Normalization

Observation system for early warning of HAB events

Alabama Department of Environmental Management Auburn / Opelika Intensive Fecal Coliform Study January February 2007

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

Predicting Tropical Cyclone Genesis

Diatoms as environmental indicators in Barnegat Bay

District of Lake Country

manuscript associated with each of your comments are described below. Your comments are in bold

Dr. Steven Koch Director, NOAA National Severe Storms Laboratory Chair, WRN Workshop Executive Committee. Photo Credit: Associated Press

3/30/2012. Two Contrasting but Complementary Evolutionary Perspectives on Human Behavior:

Simplicity is Complexity in Masquerade. Michael A. Savageau The University of California, Davis July 2004

Earth Observation and GEOSS in Horizon Copernicus for Raw Material Workshop 5 th September 2016

The Chesapeake Bay Ecological Prediction System

In-situ monitoring of RO membranes using electrical impedance spectroscopy: Threshold fluxes and fouling

SABINE RIVER AUTHORITY OF TEXAS

Synthesis and Integrated Modeling of Long-term Data Sets to Support Fisheries and Hypoxia Management in the Northern Gulf of Mexico

INTEGRATED COASTAL MONITORING OF ENVIRONMENTAL PROBLEMS IN SEA REGION AND THE WAYS OF THEIR SOLUTION

Short term PM 10 forecasting: a survey of possible input variables

Alps Results from the ESPON Project. Common spatial perspectives for the Alpine area. Towards a common vision

AUTOMATED METERED WATER CONSUMPTION ANALYSIS

The Evolutionary Biology Of Plants By Karl J. Niklas READ ONLINE

Caribbean Early Warning System Workshop

IV ASSESSING REGIME SHIFTS IN ECOSYSTEM EXPERIMENTS. Introduction. It is easier to test for multiple regimes in long-term data if the ecosystems are

Using Satellite Data to Monitor Sediment Fluxes, Water Properties and Particles Distribution in the Black Sea-Danube Interaction Zone

Department of Geography: Vivekananda College for Women. Barisha, Kolkata-8. Syllabus of Post graduate Course in Geography

Operational Perspectives on Hydrologic Model Data Assimilation

Harmful Algal Blooms (HABs) 5 Applications

Coastal Water Quality Monitoring in Cyprus using Satellite Remote Sensing

Feasibility Study for Early Warning Systems for Algae-induced Tastes and Odors. Final Report

Key abiotic and biotic determinants of occurrence and toxicological imapct of cyanobacterial blooms in a lowland dam reservoir of Sulejów, Poland

Causal Mechanisms and Process Tracing

Grouped time-series forecasting: Application to regional infant mortality counts

UC Berkeley Technical Completion Reports

RSMC-Miami Update Daniel Brown Warning Coordination Meteorologist

R021. BioTector TOC Analyzer Reagents_Mixer Reactor Systems

ECOSTAT nutrient meeting ( ) Session 1: Comparison of European freshwater and saline water nutrient boundaries

FORECASTING: A REVIEW OF STATUS AND CHALLENGES. Eric Grimit and Kristin Larson 3TIER, Inc. Pacific Northwest Weather Workshop March 5-6, 2010

Short-Term Demand Forecasting Methodology for Scheduling and Dispatch

CHAPTER 5 - QUEENSLAND FORECASTS

The Role of the SURA Testbed in the Improvement of U.S. Coastal and Estuarine Prediction

Stochastic Decision Diagrams

Regional Flash Flood Guidance and Early Warning System

Remote Sensing for Ecosystems

Applications of Isotopic Fingerprinting

Schweizerische Eidgenossenschaft Confédération suisse Confederazione Svizzera Confederazium svizra

PREDICTING SARGASSUM WASHING ASHORE IN THE LESSER ANTILLES.

To Predict Rain Fall in Desert Area of Rajasthan Using Data Mining Techniques

RADAR Rainfall Calibration of Flood Models The Future for Catchment Hydrology? A Case Study of the Stanley River catchment in Moreton Bay, Qld

Building A Weather-Ready Nation

If you have any comments or questions regarding the IMOS Bulletin please contact IMOS Communications,

Lectures on Medical Biophysics Department of Biophysics, Medical Faculty, Masaryk University in Brno. Biocybernetics

Turbidity triggers larval release by the intertidal barnacle Semibalanus balanoides

Gary G. Mittelbach Michigan State University

New design rainfalls. Janice Green, Project Director IFD Revision Project, Bureau of Meteorology

AN OVERVIEW OF THE PROCESSES AND METHODOLOGY USED BY THE SYSTEM OPERATOR TO PREPARE THE FORECAST OF DEMAND.

Hydroclimatic Variability and Change: Issues in the Intermountain West

MEMBRANE SURFACE PLANT MONTHLY OPERATIONAL REPORT TO ALABAMA DEPARTMENT OF ENVIRONMENTAL MANAGEMENT MONTGOMERY, ALABAMA.

CSLAP 2013 Lake Water Quality Summary: Lake George

A paleolimnological investigation of phytoplankton trends in a narrow rivervalley

Coordinating Multiple Model Predictive Controllers for Water Reservoir Networks Operation

BENCH TOP INSTRUMENTS DELTA OHM

WEATHER DEPENENT ELECTRICITY MARKET FORECASTING WITH NEURAL NETWORKS, WAVELET AND DATA MINING TECHNIQUES. Z.Y. Dong X. Li Z. Xu K. L.

During photosynthesis, energy from the Sun interacts with matter on Earth.

Bathymetric Survey and Sediment Hydroacoustic Study of Canyon Lake. Michael Anderson UC Riverside

Rigorous Science - Based on a probability value? The linkage between Popperian science and statistical analysis

Rigorous Science - Based on a probability value? The linkage between Popperian science and statistical analysis

Improving Biosurveillance System Performance. Ronald D. Fricker, Jr. Virginia Tech July 7, 2015

Complex Cascade Dams Operation The Glommen and Laagen Case

Rigorous Science - Based on a probability value? The linkage between Popperian science and statistical analysis

Stochastic Hydrology. a) Data Mining for Evolution of Association Rules for Droughts and Floods in India using Climate Inputs

Avoiding Nutrient Applications During Critical Periods with a Real-time Decision Support Tool: Wisconsin s Runoff Risk Advisory Forecast (RRAF)

The Kentucky Mesonet: Entering a New Phase

Nonlinear Temperature Effects of Dust Bowl Region and Short-Run Adaptation

Variation of Water Temperature and the dominant thermal stratification and vertical mixing process involved in a large,shallow lake

USEPA National Watershed Protection Program NY/NJ Harbor Estuary Program USEPA Region 2 New York, New York. USEPA Contract EP-C

The Latest Science of Seasonal Climate Forecasting

Changing Climate. An Engineering challenge for today and the future. Milwaukee School of Engineering December 2, 2015

Transcription:

Inductive reasoning and prediction of population dynamics of Cylindrospermopsis in the Wivenhoe Reservoir by means of evolutionary computation Friedrich Recknagel 1, Philip Orr 2 and Hongqing Cao 1 1 School of Earth and Environmental Sciences, University of Adelaide 2 South East Queensland Water, Brisbane

Background The presentation is based on outcomes of the ARC Linkage Project LP99453 Early warning of cyanobacteria blooms in drinking water reservoirs by means of evolutionary algorithms in collaboration with South East Queensland Water and the SA Water Corporation The research is focusing on predictive modelling of population dynamics of Anabaena, Microcystis and Cylindrospermopsis in the Myponga Reservoir, South Australia and the Wivenhoe Reservoir, Queensland We show only results for Cylindrospermopsis raciporskii in the Wivenhoe Reservoir.

Key hypotheses of the project are: - early warning of cyanobacteria blooms requires operational models driven by in situ data from online monitoring - operational in situ models can be developed by nonlinear inductive evolutionary computation - nonlinear inductive models reveal predictor variables as well as relationships and thresholds triggering cyanobacteria blooms

Inductive versus deductive modelling REALISM Explanatory Models Linear Induc.ve Deduc.ve Predictive Models Nonlinear Induc.ve Analy.cal Models Generic Models Levin, R., 1966. The strategy for model building in population biology. American Sc. 54, 421-431.

Nonlinear inductive modeling by evolutionary computation

Nonlinear inductive modeling by evolutionary computation

Wivenhoe Reservoir, Queensland 146 1825 219 2555 292 3285 365 415 438 2 1 1 365 73 195 146 1825 219 2555 292 3285 365 415 438 15 1 1 5 1 365 73 195 146 1825 219 2555 292 3285 365 415 438.15.1.5.5 365 73 195 146 1825 219 2555 292 3285 365 415 438 25 12 1 15 8 1 6 4 5 14 2 2 365 1999 73 195 21 146 1825 23 219 2555 25 292 3285 27 365 29 415 438 DO mg/l 195 Silica mg/l 73 TP mg/l WT C Turb NTU 365 2 2 TN mg/l ph 5 EC µs/cm 5 3 Chl_a μg/l max vol: 1165 Gl, max depth: 79 m; thermally stratified Dam Wall Station: historical Data 1/1999 12/21 1

365 73 195 146 1825 219 2555 292 3285 365 415 438 365 73 195 146 1825 219 2555 292 3285 365 415 438 365 73 195 146 1825 219 2555 292 3285 365 415 438 365 73 195 146 1825 219 2555 292 3285 365 415 438 (including Chl_a) 7- DAYS- AHEAD (excluding Chl_a) 7- DAYS- AHEAD Historical Data All Inputs (1/99 12/21) 2 15 1 5 Measured Predicted r 2 =.58 18 16 14 12 1 8 6 4 Measured Predicted r 2 =.57 2 Historical Data Electron. Meas. Inputs(1/99 12/21) 18 16 14 12 1 8 6 4 2 Measured Predicted r 2 =.57 18 16 14 12 1 8 6 4 2 Measured Predicted r 2 =.57

Historical Data All Inputs (1/99 12/21) (including Chl_a) IF WT>26.3 THEN Cylindrospermopsis=exp(pH+pH*81.1/(Cond+pH)) ELSE Cylindrospermopsis=(Cond+5.6)*(Chla- TP) r 2 value=.58 (excluding Chl_a) IF Turb<=57.4 AND Turb>=23.44 THEN Cylindrospermopsis=exp(WT/2.979)+WT ELSE Cylindrospermopsis=exp(WT/(11.4- ph))*(exp(turb/49.5)- TN*silica+silica) r 2 value=.57 Historical Data Elec. Meas. Inputs (1/99 12/21) IF WT<=25.5 THEN Cylindrospermopsis=(Cond*Turb/192.2- Turb)*Chla*82.5 ELSE Cylindrospermopsis=exp(pH)*exp(pH)/(Cond*Cond)*147.9 r 2 value=.57 IF WT>25.6 AND WT<32.7 THEN Cylindrospermopsis=exp(pH)*pH/(Cond- 198.8)*1.2 ELSE Cylindrospermopsis=(ln( DO )*Turb/WT+.3)*exp(pH) r 2 value=.57

365 73 195 146 1825 219 2555 292 3285 365 415 438 365 73 195 146 1825 219 2555 292 3285 365 415 438 365 73 195 146 1825 219 2555 292 3285 365 415 438 365 73 195 146 1825 219 2555 292 3285 365 415 438 Historical Data All Inputs (1/99 12/21) 8 7 6 5 4 3 2 1 (including Chl_a) THRESHOLDS WT>26.3 WT<=26.3 14 12 1 8 6 4 2 (excluding Chl_a) THRESHOLDS 23.3<=TURB<=57.4 23.3>TURB>57.4 Historical Data Elec. Meas. Inputs (1/99 12/21) 1 8 6 4 2 WT<=25.5 WT>25.5 1 8 6 4 2 25.6<WT<32.7 25.6<=WT>32.7

Historical Data All Inputs (1/99 12/21) Historical Data Elec. Meas. Inputs (1/99 12/21) 1 8 6 4 2 25 2 15 1 5 (including Chl_a) THEN- Branch ELSE- Branch Cond:22.7~477.3 ph:7.7~9 6 5 4 3 2 1 Cond:23.6~54.4 Chla:.4~15.3 TP:~.5 5 1 5 1 Cond:195.2~51.1 & 6 Cond:244.9~486.5 Chla:.1~15.6 ph:7.8~8.8 5 Turb:~38.7 4 5 1 3 2 1 5 1 14 12 1 8 6 4 2 8 7 6 5 4 3 2 1 (excluding Chl_a) THEN- Branch ELSE- Branch WT:14.2~27.9 25 2 15 1 5 5 1 16 Cond:245.1~486.3 14 ph:7.8~8.8 12 5 1 1 8 6 4 2 ph:7.4~8.7 Turb:~39.4 WT:16.6~3.2 silica:~8.5 TN:.3~.7 5 1 DO:5.3~11.8 ph:7.3~8.9 Turb:~38.8 WT:15.2~27 5 1

4 ph 36 72 2 18 DO mg/l 2 1 1 36 72 5 18 4 4 3 3 2 2 1 1 36 72 18 7 6 5 4 3 2 1 36 27 72 28 18 29 21 Chl_a μg/l WT C 5 2 5 Turb NTU 1 6 3 max vol: 1165 Gl, max depth: 79 m; thermally stratified Dam Wall Station: Online Data 9/27 12/21 EC µs/cm Wivenhoe Reservoir, Queensland

365 73 195 146 1825 219 2555 292 3285 365 415 438 365 73 195 146 1825 219 2555 292 3285 365 415 438 36 72 18 365 73 195 146 1825 219 2555 292 3285 365 415 438 365 73 195 146 1825 219 2555 292 3285 365 415 438 36 72 18 (including Chl_a) 7- DAYS- AHEAD (excluding Chl_a) 7- DAYS- AHEAD Historical Data All Inputs (1/99 12/21) 2 15 1 5 Measured Predicted r 2 =.58 18 16 14 12 1 8 6 4 Measured Predicted r 2 =.57 2 Historical Data Electron. Meas. Inputs(1/99 12/21) 18 16 14 12 1 8 6 4 2 Measured Predicted r 2 =.57 18 16 14 12 1 8 6 4 2 Measured Predicted r 2 =.57 Online Data (9/27 to 12/21) 8 7 6 5 4 3 2 1 Measured Predicted r 2 =.65 8 7 6 5 4 3 2 1 Measured Predicted r 2 =.68

Historical Data All Inputs (1/99 12/21) (including Chl_a) IF WT>26.3 THEN Cylindrospermopsis=exp(pH+pH*81.1/(Cond+pH)) ELSE Cylindrospermopsis=(Cond+5.6)*(Chla- TP) r 2 value=.58 (excluding Chl_a) IF Turb<=57.4 AND Turb>=23.44 THEN Cylindrospermopsis=exp(WT/2.979)+WT ELSE Cylindrospermopsis=exp(WT/(11.4- ph))*(exp(turb/49.5)- TN*silica+silica) r 2 value=.57 Historical Data Elec. Meas. Inputs (1/99 12/21) IF WT<=25.5 THEN Cylindrospermopsis=(Cond*Turb/192.2- Turb)*Chla*82.5 ELSE Cylindrospermopsis=exp(pH)*exp(pH)/(Cond*Cond)*147.9 r 2 value=.57 IF WT>25.6 AND WT<32.7 THEN Cylindrospermopsis=exp(pH)*pH/(Cond- 198.8)*1.2 ELSE Cylindrospermopsis=(ln( DO )*Turb/WT+.3)*exp(pH) r 2 value=.57 Online Data (9/27 to 12/21) IF WT_online<25.7 THEN Cylindrospermopsis=(WT_online- 25.2)* (ph_online+chla_online)*98.5+3868.6 ELSE Cylindrospermopsis=(exp(pH_online)+562.1)* ln( (Chla_online- 14) )- (Conduc.vity_online- ph_online* 44.5-68.3)*115.3 r 2 value=.65 IF Conduc.vity_online<=296.5 THEN Cylindrospermopsis=(((Conduc.vity_online+ Turbidity_online)+Turbidity_online)*(WT_online- 16.1)) ELSE Cylindrospermopsis=((((WT_online+(- 1.9))*82.5)- (Conduc.vity_online+(Conduc.vity_online+135.1)))*(WT_online+ (exp(ph_online)/(conduc.vity_online+ph_online)))) r 2 =.68

365 73 195 146 1825 219 2555 292 3285 365 415 438 365 73 195 146 1825 219 2555 292 3285 365 415 438 36 72 18 365 73 195 146 1825 219 2555 292 3285 365 415 438 365 73 195 146 1825 219 2555 292 3285 365 415 438 36 72 18 (including Chl_a) THRESHOLDS (excluding Chl_a) THRESHOLDS Historical Data All Inputs (1/99 12/21) 8 7 6 5 4 3 2 1 WT>26.3 WT<=26.3 14 12 1 8 6 4 2 23.3<=TURB<=57.4 23.3>TURB>57.4 Historical Data Elec. Meas. Inputs (1/99 12/21) 1 8 6 4 2 WT<=25.5 WT>25.5 1 8 6 4 2 25.6<WT<32.7 25.6<=WT>32.7 Online Data (9/27 to 12/21) 6 5 4 3 2 1 WT<25.7 WT>=25.7 5 4 3 2 1 EC > 296.5 EC <= 296.5

Historical Data All Inputs (1/99 12/21) Historical Data Elec. Meas. Inputs (1/99 12/21) Online Data (9/27 to 12/21) 1 8 6 4 2 25 2 15 1 5 7 6 5 4 3 2 1 (including Chl_a) THEN- Branch ELSE- Branch Cond:22.7~477.3 ph:7.7~9 6 5 4 3 2 1 3 2 1 Cond:23.6~54.4 Chla:.4~15.3 TP:~.5 5 1 5 1 Cond:195.2~51.1 & 6 Cond:244.9~486.5 Chla:.1~15.6 ph:7.8~8.8 5 Turb:~38.7 4 5 1 WT_online:15.1~27.1 5 ph_online:7~9 Chla_online:.8~11.7 4 5 1 3 2 1 5 1 Conduc.vity_online: 241~498 ph_online:7.7~9.4 Chla_online:~17.5 5 1 14 12 1 8 6 4 2 8 7 6 5 4 3 2 1 4 3 2 1 (excluding Chl_a) THEN- Branch ELSE- Branch WT:14.2~27.9 25 2 15 1 5 5 1 16 Cond:245.1~486.3 14 ph:7.8~8.8 12 5 1 WT_online:15.1~26.4 Conduc.vity_online: 24~311 Turbidity_online:~7.4 5 1 1 8 6 4 2 4 3 2 1 ph:7.4~8.7 Turb:~39.4 WT:16.6~3.2 silica:~8.5 TN:.3~.7 5 1 DO:5.3~11.8 ph:7.3~8.9 Turb:~38.8 WT:15.2~27 5 1 WT_online:16.1~3.7 Conduc.vity_online: 269.8~54.6 ph_online:7.3~9.1 5 1

Towards in situ operational models for early warning of cyanobacteria blooms Early Warning Horizon Operational Control Horizon Strategic Control Horizon Sampling Time days weeks seasons/years t t + T s Nonlinear Inductive Models Deductive Models

Towards in situ operational models for early warning of cyanobacteria blooms Data Archiving in the Ecological Data Warehouse On-line Data Historical Data Water Temperature C Diss. Oxygen mg/l Real-time in situ Water Quality Measurements by Hydrolab DataSonde 5X Turbidity NTU ph Ammonium NH 4 mg/l Conductivity ms/cm Total Chlorophyll µg/l Data Acquisition by Hydrolab Process Monitor On-line Data Data Merger and Validation Phycocyanoin µg/l Early Warning for Operational Raw Water Control if Algal Bloom is Imminent Chlorophyll-a µg/l Anabaena circinalis cells/ml Microcystis cells/ml Data Preprocessing Module Real-Time Forecasting Forecasting Module Model Model Design Time Series

Towards operational models for early warning of cyanobacteria blooms http://lakedataweb.services.adelaide.edu.au/ldw.aspx

What s next? Spatially-explicit forecasting of cyanobacteria assemblages in drinking water reservoirs by multi-objective evolutionary computation Turb NTU Wivenhoe Reservoir: 6 monitoring stations

What s next? Spatially-explicit forecasting of cyanobacteria assemblages in drinking water reservoirs by multi-objective evolutionary computation

Conclusions: -Nonlinear inductive models by evolutionary computation inform about ecological relationships and thresholds determining cyanobacteria population dynamics - Nonlinear inductive models by evolutionary computation provide short-term forecasting of cyanobacteria population dynamics - Nonlinear inductive models by evolutionary computation suit as in situ operational models for early warning of outbreaks of cyanobacteria blooms -Multi-objective evolutionary computation allows to develop models for spatially-explicit forecasting of cyanobacteria assemblages across sampling stations in lakes

Acknowledgements: We thank the ARC, SEQWater and SA Water for providing funding, and thank SEQWater and SA Water for their constructive support.

Early Warning of Cyanobacteria Blooms NORMAL WARNING ALARM

Early Warning of Cyanobacteria Blooms NORMAL WARNING ALARM

Early Warning of Cyanobacteria Blooms NORMAL WARNING ALARM

Inductive versus deductive modelling Ecological, Economic and Social Sciences Medicine Engineering Physics Nonlinear Inductive Models Deductive Models Electrical Circuits Inductive Models Karplus, W.J., 1983. The spectrum of mathematical models. Perspectives in Computing 3, 2, 4-13.