Ecological Modeling: Algae -Why? - Who? - What? - How?

Slides:



Advertisements
Similar presentations
Individual-based Models Three Examples
Advertisements

A Modeling Analysis of the Clear Water Phase CE Surface Water Quality Modeling Case History.
A Recipe for Ocean Productivity, with Variations John Marra Lamont-Doherty Earth Observatory Palisades, NY USA.
Assimilation Numbers?? Phytoplankton Absorption: a Strong Predictor of Primary Productivity in the Surface Ocean Or: Throw Away that Lab Fluorometer John.
Functional traits, trade-offs and community structure in phytoplankton and other microbes Elena Litchman, Christopher Klausmeier and Kyle Edwards Michigan.
The material in this slide show is provided free for educational use only. All other forms of storage or reproduction are subject to copyright- please.
The Open Shelf Sea. 1. The primary source of buoyancy is surface heat flux. c p = specific heat capacity of seawater (= 3900 J kg -1 K -1 ) mean water.
Individual organism: How do structure, physiology, and behavior lead to the individual’s survival and reproduction? Population: What determines the number.
© 2011 Pearson Education, Inc. CHAPTER 13 Biological Productivity.
Succession in a water column An adapting ecosystem maneuvering between autotrophy and heterotrophy Jorn Bruggeman Theoretical biology Vrije Universiteit.
LIGHT/VERTICAL MIXING The prevailing role of light in the Southern Ocean was inferred from the weak vertical stability of surface waters and the strong.
Modelling the export of biogenic particulates from upper ocean Philip Boyd.
Basic Ecology I Energy Types of Ecosystems Productivity Energy Flow Trophic levels Food webs/chains.
OC211(OA211) Phytoplankton & Primary Production Dr Purdie SOC (566/18) LECTURE 6 Week 6 (i) Photosynthesis & Light (ii) Critical.
Lecture Goals To review the concept of trophic structure – how energy moves through ecosystems. To discuss primary production in freshwater ecosystems.
I.Intro: Plant responses to elevated CO 2 ? II. Resource limitations of photosynthesis A. CO2 response B. Nutrient response C. Light response curves and.
Prof. Heidi Fuchs
Open Oceans: Pelagic Ecosystems II
Inorganic Nutrient Availability & Phytoplankton Growth: the start of Biogeochemical Cycles Re-read pp , Habitat Determinants of Primary Production.
Diversity of Aquatic Organisms Phytoplankton & Phytoplankton Ecology Part 3.
Phytoplankton: Nutrients and Growth. Outline Growth Nutrients Limitation Physiology Kinetics Redfield Ratio Critical Depth.
Ocean Biology: Phytoplankton in Biospheric Processes.
EVPP 550 Waterscape Ecology and Management – Lecture 9 Professor R. Christian Jones Fall 2007.
Plot of increases in cell number vs time for cell dividing by binary fission = Growth Curve Logarithmic Growth N = No2 n N = No2 n Exponential Growth N.
©2010 Elsevier, Inc. Chapter 17 Nutrient Use and Remineralization Dodds & Whiles.
Trait-based representation of diatom diversity in a Plankton Functional Type model N. T ERSELEER 1, J. B RUGGEMAN 2, C. L ANCELOT 1 AND N. G YPENS 1 1.
OUR Ecological Footprint The hierarchical nature and processes of different levels of ecological systems:
Phytoplankton bloom – there is no officially recognized threshold level –range from 10,000s – 1,000,000s of cells per ml.
IoE The Basics of Satellite Oceanography. 7. Ocean Color and Phytoplankton Growth Lecture 7 Ocean Color and Phytoplankton Growth.
Chapter 54 Ecosystems. An ecosystem consists of all the organisms living in a community as well as all the abiotic factors with which they interact Ecosystems.
Prof. Heidi Fuchs Suggestions for getting an A How to deal with equations? –Don’t panic! –If you understand an equation, you.
Third annual CarboOcean meeting, 4.-7.December 2007, Bremen, Segschneider et al. Uncertainties of model simulations of anthropogenic carbon uptake J. Segschneider,
Module 2 Biocomplexity of the North Dactylica arctica Algae under Arctic sea ice Xanthoria elegens Poripidia flavocaerulescens.
Phytoplankton: Nutrients and Growth. Outline Growth Nutrients Limitation Physiology Kinetics Redfield Ratio (Need to finish today) Critical Depth (Sally.
© 2014 Pearson Education, Inc.. Primary Productivity Rate at which energy is stored in organic matter –Photosynthesis uses solar radiation. –Chemosynthesis.
Modelling Crop Development and Growth in CropSyst
Sensing primary production from ocean color: Puzzle pieces and their status ZhongPing Lee University of Massachusetts Boston.
Quantifying Microorganisms and Their Activity CE 421/521 Environmental Biotechnology Lecture for September 19, 2006 Vaccari et al., Chapter 10.
PATTREN OF PRIMARY PRODUCTION
Modelling 2: Introduction to modelling assignment. A basic physical-biological model. Model equations. Model operation. The assignment.
with contributions from:
Doney, 2006 Nature 444: Behrenfeld et al., 2006 Nature 444: The changing ocean – Labrador Sea Ecosystem perspective.
Natural Selection in a Model Ocean
Upstate Freshwater Institute Markensten et al. NYWEA 2008 Simulating multiple functional groups of phytoplankton in Cannonsville Reservoir Hampus Markensten.
Ecology: Human Impacts David Mellor, PhD Citizen Science Coordinator Virginia Master Naturalists.
Simulation labs for Biology 4263 I gave an introductory lab talk on Keystone Predators and Barnacles and Tides on Thursday, April 16 th. These labs are.
Ecology --- primary definition The scientific study of how organisms interact with the natural world.
Primary production & DOM OUTLINE: What makes the PP levels too low? 1- run Boundary conditions not seen (nudging time) - Phytoplankton parameter:
Microbial kinetics of growth and substrate utilization. Batch culture and Kinetics of Microbial growth in batch culture After inoculation the growth rate.
Daoxun Sun Outline Background Data Technical details Result EOF of chlorophyll data Correlation with possible factors Summary.
Microbial Kinetics and Substrate utilization in Fermentation
Sandia is a multiprogram laboratory operated by Sandia Corporation, a LockheedMartin Company, for the United States Department of Energy’s National Nuclear.
Biology of mixed layer Primary production by Phytoplankton - small drifting organisms that photosynthesize Competition and limits on production Critical.
Biological Productivity in the Ocean
Competition for nutrients Major phytoplankton groups Light
Suggestions for getting an A
Critical and Compensation Depths (refer to handouts from 9/11/17)
Puget Sound Oceanography
Primary Production and Satellite Remote Sensing
Fig. 1. Relationship between maximal growth rates and cell sizes of phytoplankton taken from various sources in the literature, measured at or recalculated.
Marine Botany Lesson 4 (continued from last week): The physical and chemical environment relevant to marine plant growth in the oceans…
Primary Producers Algae – microscopic plankton (and benthic)
Neuse Estuary Eutrophication Model
What is Productivity? Amount of solar energy provided to an ecosystem
Primary Production and the Function of Organisms in the Process
Eutrophication Processes
Biology of mixed layer Primary production
Critical and Compensation Depths Spring bloom and seasonal cycle
Presentation transcript:

Ecological Modeling: Algae -Why? - Who? - What? - How?

Who? Who?

What? What?

Examples of Models with Algal Modeling Included CIAO- Coupled Ice Atmosphere Ocean Model CIAO- Coupled Ice Atmosphere Ocean Model ERSEM- European Regional Seas Ecosystem Model ERSEM- European Regional Seas Ecosystem Model CE QUAL CE QUAL DSSAMt DSSAMt HSPF HSPF WASP WASP Aquatox Aquatox Ecosim Ecosim FFFMSIPaAG, FFFMSIPaAG, John’s Model, John’s Model, Don’s model Don’s model …………..Yada, Yada, Yada, …………..Yada, Yada, Yada,

What is typically modeled? - Phytoplankton - Periphyton

Pennate Diatoms

Centric Diatoms

Filamentous Green Algae

Chrysophyte

Cryptophyte

Dinoflagellates

Filamentous Cyanobacteria

Coccoid Cyanobacteria

Red Algae

Brown Algae

The point is that is…. it is a Diverse “Group” – –Size (pico, nano,micro) – –Physiologically – –Biochemically – –Life Histories – –And Therefore, Ecosystem Function!!

The How: Algal Population Growth Formula dA/dt =  max (T)A*MIN(NLIM)* LightLIM - grazing +/- advection/dispersion +/- settling Be a bit skeptical: ask can the equations capture “algal” physiologies and community dynamics that you are after?

uMax Usually set by Temperature: Usually set by Temperature: –Eppley 1972 (most common*) Other approaches Other approaches –species-genera specific temperature relationships – Multiple T opt, T max T min, fxns Temperature ( o C)  max Temperature ( o C)  max

Nutrient Limitation Monod kinetics Monod kinetics Usually applied as the single most limiting nutrient (Leibig’s “Law of The Minimum” improperly invoked). Usually applied as the single most limiting nutrient (Leibig’s “Law of The Minimum” improperly invoked). –Half saturation coefficients (ks) and nutrient concentrations are all that are needed.   =  max *(N/(K s +N)

Challenges: –How to set the K s. –What nutrient concentration to use: bulk or microscale? Half Saturation Constants Figure 1. Model formulation for velocity enhancement in DSSAMt (Caupp et al 1998). Figure 2. Predictions from biofilm theory using hypothetical model parameters.

Light Photosynthesis versus Irradiance Curves (PE curves) Photosynthesis versus Irradiance Curves (PE curves) –E k is needed. Challenges: Challenges: –How to calculate effective E. –How to set E k (remember….. plants/algae physiologically adapt). EkEkEkEk P max

Effective E: Effective E: –Typically Calculated by 1 st order attenuation accounting for water+ constituents –E d or E od, or E o ? –PAR, PUR, or PHAR?

Integrate over depth and time for applicable Dt. Integrate over depth and time for applicable Dt. WASP 6 manual

Note: dA/dt =  max(T)A*MIN(NLIM)* LightLIM This is “net primary production” Also, this is the “net cellular growth rate” Equation readily allows addition of other environmental constraints such as salinity, pH, etc….

Grazing Zero Order loss term/Constant Zero Order loss term/Constant First order loss term First order loss term Kinetics based on constant grazer biomass/abundance but accounts for monod kinetics Kinetics based on constant grazer biomass/abundance but accounts for monod kinetics Kinetics with grazer abundance predicted as well (Lotkka- Volterra, NPZ models) Kinetics with grazer abundance predicted as well (Lotkka- Volterra, NPZ models)

Other losses…. Settling? Settling? Mortality- Mortality- –Viral, fungal, Ecotox pollutants (e.g. phototoxins, LD 50 ’s) other..? Drift/scour (fxn velocity and biomass) Drift/scour (fxn velocity and biomass)

Algal Algorithms embedded in spatial models Algal Algorithms embedded in spatial models

Still Not Very Satisfying.... Uncertainties in Temperature and  max Uncertainties in Temperature and  max –can lead to large variations in accumulation rates and biomass.. (exponentially compounding uncertainty) Treatment of K s ’s and E k ’s as constants Treatment of K s ’s and E k ’s as constants Transient luxury uptake of nutrients rarely accounted for (e.g. Carbon storage and growth at night, i.e. “unbalanced” growth). Transient luxury uptake of nutrients rarely accounted for (e.g. Carbon storage and growth at night, i.e. “unbalanced” growth). Minimal Constraints on loss terms Minimal Constraints on loss terms Stability issues Stability issues

Other Approaches… More Empirical Relationships More Empirical Relationships –e.g. TP vs. Chlorophyll a Quantum Yield Approach Quantum Yield Approach –E o *A*  = Primary Production

Free stuff I (Heather/Laurel) will post Stella models I (Heather/Laurel) will post Stella models Download isee Player (its free) Download isee Player (its free)

Background Readings Eppley 1972 Eppley 1972 Chapra pages Chapra pages Brush et al Brush et al Chapra (Solar Radiation and light extinction sections) Chapra (Solar Radiation and light extinction sections) WASP Manual WASP Manual Kirk: Light and Photosynthesis in the sea Kirk: Light and Photosynthesis in the sea Sverdrup: Conditions for phytoplankton blooms Sverdrup: Conditions for phytoplankton blooms