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NEXT GENERATION MODELS FOR PLANETARY MANAGERS Michael Barton - May 2016

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Page 1: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

NEXT GENERATION MODELS FOR PLANETARY MANAGERS

Michael Barton - May 2016

Page 2: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

A HUMANIZED PLANET

> 50% of land in crops or pasture

Page 3: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

A HUMANIZED PLANET

> 50% of land in crops or pasture

> 50% of forests cleared; more reforested

Page 4: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

A HUMANIZED PLANET

Humans plus agro-biomass >3 billion tons

More than all other vertebrates combined (land and sea)

(XKCD 3/5/14)

Page 5: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

A HUMANIZED PLANET

Coastlines engineered

Page 6: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

A HUMANIZED PLANET

Coastlines engineered

> 50% of fresh water used and 6x more water stored

Page 7: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

A HUMANIZED PLANET

Coastlines engineered

> 50% of fresh water used and 6x more water stored

More N cycled

Page 8: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

A HUMANIZED PLANET

Coastlines engineered

> 50% of fresh water used and 6x more water stored

More N cycled

More sediment transported

Page 9: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

A HUMANIZED PLANET

Humanity is more than a global keystone species

Ruddiman et al 2016

Page 10: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

A HUMANIZED PLANET

Humanity is more than a global keystone species

Our planetary environment shaped by human decisions, technology, and nature

Ruddiman et al 2016

Page 11: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

A HUMANIZED PLANET

Humanity is more than a global keystone species

Our planetary environment shaped by human decisions, technology, and nature

Human impacts can exceed non-human forces

Previous analyses showed a difference between the Holocene δ18O response and those during interglacialstages 5, 7, and 9 [Ruddiman, 2007]. That assessment is updated in Figure 2d to include interglaciations priorto stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000 years, whereastrends in most previous interglaciations (except stage 15) move toward more “glacial” conditions (colderdeep-ocean temperatures and/or greater ice volume). As a result, the average δ18O trend for the previousinterglaciations differs from the Holocene signal (Figure 3d). A newer compilation for the Holocene showsno significant δ18O change from 7000 years ago to the present [Stern and Lisiecki, 2015].

Along with the average trends of all four signals during previous interglaciations, Figure 3 shows a onestandard deviation envelope. In each case, the Holocene signal moves outside this envelope during the last1 or 2 millennia. Most of this envelope of variation is not caused by sample-to-sample noise withininterglaciations, but by the widely varying ranges of the signal among the interglaciations, likely due todifferences in orbital forcing.

As noted above, the trends in Figures 2 and 3 are aligned on the first esinωmaximumwithin each interglacia-tion. In contrast, two other methods aligned stage 1 with previous interglacial stage 11 using the start of thepreceding deglaciations defined by δD trends [EPICA Community Members, 2004] and by CO2 signals [Broeckerand Stocker, 2006].

In contrast to these choices, the signal most commonly used to define past glacial-interglacial cycles is thebenthic δ18O record [Lisiecki and Raymo, 2005], which is used in Figure 4 to align all deglaciations. Thedeglaciation preceding the Holocene (as well as those prior to interglacial stages 5, 7, 9, and 19) lasted about

Figure 3. Comparison of Holocene trends (red) to stacked averages for previous interglaciations (blue). The light blueshading shows one standard deviation. (a) CH4, (b) CO2, (c) δD, and (d) δ18O from sources listed in Figure 2 caption. DomeC CO2 and CH4 data for pre-Holocene interglaciations calculated by binning at 1000 year intervals. Dome C δD data calculatedas binned 500 year averages for stages 1 to 11 and by interpolation between actual values for stages 15 to 19. δ18O data for allinterglaciations are binned averages from the benthic stack [Lisiecki and Raymo, 2005]. Stage 15 is excluded in the averageshown by the solid blue line and included in the trend shown by the dashed line. Recent CO2 reanalyses [Bereiter et al., 2015]shift the previous interglacial average upward by ~1 ppm but retain the same downward trend.

Reviews of Geophysics 10.1002/2015RG000503

RUDDIMAN ET AL. THE HOLOCENE: NATURAL OR ANTHROPOGENIC? 4

all other interglacials of last 800,000 yrs

current in

terglacial

Ruddiman et al 2016

Page 12: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

A HUMANIZED PLANET

The human species has transitioned from individuals harvesting wild resources

Page 13: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

A HUMANIZED PLANET

The human species has transitioned from individuals harvesting wild resources

To communities managing local ecosystems

Page 14: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

A HUMANIZED PLANET

The human species has transitioned from individuals harvesting wild resources

To communities managing local ecosystems

And now are confronted with the need to manage our planetary systems

Page 15: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

A NEW SOCIAL REALITY

Our social life has also become global

Humankind has transformed from a normal terrestrial animal to a unique global phenomenon

Nearly 8 billion people

Over half live in urban hives of millions of individuals

Page 16: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

A NEW SOCIAL REALITY

Digital media and rapid transportation now connect humanity economically, socially, and culturally in a global network of multiple, cross-cutting ties

This has created complex social-ecological-technological systems (CSETS) at planetary scale

Page 17: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

A NEW SOCIAL REALITY

A few millennia ago, all people lived in small communities

An individual could observe social and natural phenomena and extrapolate the consequences of their actions on fellow humans and the natural world

This is no longer the case

Page 18: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

PLANETARY CSETS

Scale and complexity of our global CSETS unprecedented for any organism in earth's history

Page 19: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

PLANETARY CSETS

Scale and complexity of our global CSETS unprecedented for any organism in earth's history

CSETS multi-dimensional, multi-scale causality and non-linear dynamics exceed our innate abilities to anticipate the consequences of decision-making

Page 20: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

PLANETARY CSETS

Scale and complexity of our global CSETS unprecedented for any organism in earth's history

CSETS multi-dimensional, multi-scale causality and non-linear dynamics exceed our innate abilities to anticipate the consequences of decision-making

And human system dynamics are major drivers of Earth’s biophysical environment

Page 21: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

NEXT GENERATION SCIENCE FOR PLANETARY SOCIOECOLOGICAL SYSTEMS

In an Earth dominated by rapidly changing, telecoupled human and biophysical processes…

we need next generation data-driven science and modeling to enable us to sustainably manage dynamics of a planetary socio-ecological system

Page 22: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

NEXT GENERATION SCIENCE FOR PLANETARY SOCIOECOLOGICAL SYSTEMS

Building new capacity in data science and modeling of human systems at planetary scales poses significant challenges

Require coordinated, community-wide efforts

Need to build on existing research and alsobe willing to explore new directions

Briefly outline some of the relevant issuesand challenges

Page 23: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

MODELING GOALS

All models are wrong but some are useful (G. Box)

What kind of models are most useful - produce the most value - for scientific understanding and for planetary management?

Generative/process models vs. descriptive/empirical models

Models as experiment & scenario creation vs. replicating the planet in silico

Which behaviors or phenomena are controlled or boundary conditions?

Which are simulated?

Which can be ignored?

Page 24: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

FEEDBACKS ARE CRUCIAL

We know from abstract models and small-scale realistic simulations that…

Insignificant differences can have enormous consequences in complex systems due to cascades of interaction effects and feedbacks

Powerful forces can have negligible consequences for the same reasons

Feedbacks in CSETS should be equally important at global scales.

How can we create modeling environments that simulate feedbacks between human and biophysical processes?

Page 25: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

SPACE MATTERS…EXCEPT WHEN IT DOESN’TMuch current social science is aspatial

e.g.: individual cases studies, social networks, national surveys, economic indicators

Human action and impacts on biophysical systems are local and vary across space

But interaction effects change across scales

And electronic media have created global interaction networks where distance is irrelevant—though consequences may still be local.

How can we represent interactions of spatially-explicit social actors and distance-irrelevant information networks?

Page 26: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

DYNAMICS CROSS MULTIPLE SCALES

Climate is global, weather is local. Policies and institutions are top down, human action is bottom up.

Combined effects of many individual actions are changing climate

Climate imposes boundary conditions on weather which affects human actions

Interaction effects and feedbacks cause CSETS dynamics operate across multiple scales.

How do we model cross-scale processes and consequences

Page 27: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

WHERE & HOW TO COARSE-GRAINIn all CAS, higher level emergent properties are not easily explained or predicted from properties of individual lower level components

All biophysical and human components of CSETS composed of subatomic particles

Earth’s thermal balance can be represented in a single equation

Neither scale of analytical units or processes helpful for understanding and managing most relevant dynamics of global CSETS

Between the scales of modeling 8 billion individual agents, and aggregating all people into a single variable, what provides the most value and is most tractable?

How to downscale and coarse-grain up human systems processes and interactions at chosen scales?

Page 28: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

BIG DATA ARE SMALL DATA

Much current social science focuses on …

Few, information rich cases

Indices aggregated across a few regions

Page 29: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

BIG DATA ARE SMALL DATA

Much current social science focuses on …

Few, information rich cases

Indices aggregated across a few regions

Need to make much better use of …

Many cases with a little information in each

High-dimensional data

Integrating ontologically diverse and multi-scale data sets

Page 30: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

PRAGMATICS

How do we intellectually maintain and manage a global scientific agenda for modeling human systems?

Who writes the code? In what language?

How does modeling environment evolve?

How do we maintain standards for API or I/O and integrate them with existing ESMs?

Where can the code be run?

How do we decide which modeling experiments to run?

How do we evaluate results? (HSMIPS?)

Page 31: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

A FIRST STEP FOR NEXT GENERATION HUMAN-EARTH SYSTEMS SCIENCE

Page 32: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

A FIRST STEP FOR NEXT GENERATION HUMAN-EARTH SYSTEMS SCIENCE

Page 33: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

COMSES NETNetwork for Computational Modeling in Social & Ecological SciencesPartner with CSDMS for organizing workshop

Page 34: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

COMSES NET

NSF sponsored Research Coordination Network

A community of practice for scientists using advanced modeling to study human and natural systems

http://www.openabm.org

Page 35: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

COMSES NET

Framework for interaction and professional development

http://www.openabm.org

Page 36: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

Newly certified models in the CoMSES model library and newly published models added to the model library.

... a node in the CoMSES Network

CoMSES Digest: Fall 2015Volume 3, No.3 June 16, 2015 – September 15, 2015

This is the Fall 2015 issue of the CoMSES Digest, and it brings good news on two fronts:first, a generous number of models were uploaded and certified during the past threemonths, and downloads were high as well; second, CoMSES is hosting a conferencesession to discuss models and modeling in science and the potential collaborative roles inthis that CoMSES members can play.

Newly Certified and Newly Posted Models, Downloads Three models have been newly certified­ the largest total since the first CoMSES Digestissue. Mark Moritz and colleagues have had certified a NetLogo simulation of pastoralmobility, which they used for a paper that was published in the April 9th issue ofEcological Modeling. The model posits that given a set of assumptions about theinformation flow and decision­making processes among pastoralists sharing common­poolresources, and ideal free distribution may result. Kit Martin has has received certificationfor an earlier model in which leafcutter ants engage in intra­colony competition­ and evenkill each other­ despite being genetically related. And Shade Shutters and David Haleshave received certification for a model of the emergence of altruism in a population whereindividuals can consider themselves more or less similar to others based on 'tags', anduse these tags to determine their willingness to engage in altruistic acts. In all three cases,the model certification indicates that these models are confirmed to run as described andto be documented and accessible to the wider modeling community. For those of youteaching courses in agent­based models, socio­ecological systems modeling, orcomplexity, look to these and other certified models for good examples for your classes.

Eight new models were added to the library, covering a wide range of topics, includingvoter turnout, pedestrian movement, vehicle purchase choice, and cultural transmission,inter alia. Resource management is explored via simulation (Waring et al.) and by askingindividuals to engage in role­playing (Le Page et al.). A new implementation of

COMSES NET

Framework for interaction and professional development

Overcoming challenges to knowledge dissemination and sharing

http://www.openabm.org

Page 37: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

Newly certified models in the CoMSES model library and newly published models added to the model library.

... a node in the CoMSES Network

CoMSES Digest: Fall 2015Volume 3, No.3 June 16, 2015 – September 15, 2015

This is the Fall 2015 issue of the CoMSES Digest, and it brings good news on two fronts:first, a generous number of models were uploaded and certified during the past threemonths, and downloads were high as well; second, CoMSES is hosting a conferencesession to discuss models and modeling in science and the potential collaborative roles inthis that CoMSES members can play.

Newly Certified and Newly Posted Models, Downloads Three models have been newly certified­ the largest total since the first CoMSES Digestissue. Mark Moritz and colleagues have had certified a NetLogo simulation of pastoralmobility, which they used for a paper that was published in the April 9th issue ofEcological Modeling. The model posits that given a set of assumptions about theinformation flow and decision­making processes among pastoralists sharing common­poolresources, and ideal free distribution may result. Kit Martin has has received certificationfor an earlier model in which leafcutter ants engage in intra­colony competition­ and evenkill each other­ despite being genetically related. And Shade Shutters and David Haleshave received certification for a model of the emergence of altruism in a population whereindividuals can consider themselves more or less similar to others based on 'tags', anduse these tags to determine their willingness to engage in altruistic acts. In all three cases,the model certification indicates that these models are confirmed to run as described andto be documented and accessible to the wider modeling community. For those of youteaching courses in agent­based models, socio­ecological systems modeling, orcomplexity, look to these and other certified models for good examples for your classes.

Eight new models were added to the library, covering a wide range of topics, includingvoter turnout, pedestrian movement, vehicle purchase choice, and cultural transmission,inter alia. Resource management is explored via simulation (Waring et al.) and by askingindividuals to engage in role­playing (Le Page et al.). A new implementation of

COMSES NET

Framework for interaction and professional development

Overcoming challenges to knowledge dissemination and sharing

Publishing model code to catalyze innovation in computational modeling

http://www.openabm.org

Page 38: NEXT GENERATION MODELS FOR PLANETARY MANAGERS · to stage 9. The Holocene δ18O signal remains at full interglacial values during the last 7000years, whereas trends in most previous

COMSES NETGo to this report

Jan 1, 2015 ­ Dec 31, 2015Location

41.75%

34.91%

17.15%

3.21%

2.98%

Rows 1 ­ 5 of 5

Map Overlay

Summary

53,305% of Total: 99.50% (53,573)

53,305% of Total: 99.50% (53,573)

1. Americas 22,255

2. Europe 18,608

3. Asia 9,140

4. Africa 1,712

5. Oceania 1,590

1,5901,5901,590 22,25522,25522,255

Continent Sessions Sessions

© 2016 Google

All Users

99.50% Sessions

>1600 members

348 published models

>53,000 site visitors in 2015

>16,000 model downloads in 2015

http://www.openabm.org