ES2- 2Tues Systems

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    Read any newspaper article with a scientifically critical eye.

    What dont they tell you?What assumptions are made?

    What would they have you believe with no evidence?

    Are there discrete conclusions or are you left to infer?

    Tell the person next to you about it. - NW.

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    The Textboo! is ready" The Textboo! is ready"

    #f you didnt already order it$

    %tep &$ 'o( on to https$))students.universityreaders.com)store).

    %tep *$ +reate an account or lo( in if you have an existin(

    account to purchase.

    %tep ,$ asy-to-follow instructions will (uide you throu(h the restof the orderin( process.

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    %%T/$ A set of components that function to(ether as one.

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    0eedbac! is the response of part of a system to chan(e in or

    information from another.

    1 2ositive feedbac!$ tends to amplify the stimulus or chan(example- compound interest

    1 Ne(ative feedbac!$ tends to reduce or dampen chan(e

    xample- friction

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    2ositive 0eedbac!

    Ne(ative 0eedbac!

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    3A#%WR'3

    Albedo$ 4bri(htness5 of surface. 0raction of li(ht reflected.

    Water dar!est6 then forest6 then (rass6 desert6 ice.

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    A chan(e in one part of the system affects the behavior of

    other components within the system.

    1 3ia(nostic challen(e

    -+hic!en and e(( problem

    1 2otential positive feedbac!s-Runaway chan(e and collapse

    1 2ositive feedbac!s may mas! chan(e

    -Not observed until too late

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    bservation$ woodland chan(ed to (rassland7ypothesis$ +attle (ra8in( and elephant dama(e !illed trees

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    /asai (ra8in( (oats

    lephants

    dama(e trees

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    Test 7ypothesis

    #s tree loss proportional to amount of (ra8in(?Number of elephants?

    No.

    %o what other factors are there in the system?

    Rainfall increased. 7mmm9

    %alt from la!e bed soil rose to tree roots- !illed trees

    lephants compounded the problem

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    2olar ice and temperature

    -As ice melts6 white is replaced by blac! water

    -absorbs more sunli(ht

    -increases temperature

    -melts faster9

    :pposite of 3aisy-world;

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    Desertification of Sahara

    -%unli(ht was decreasin( in intensity due to orbital chan(es

    -3ar! ve(etation warmed re(ion and !ept moisture in system

    -ventually could not 4!eep up5 with decreasin( insolation

    -cosystem collapsed

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    2ositive feedbac!s can become ne(ative6 !eepin( the

    system within bounds.

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    xponential (rowth if rate of increase is proportional to

    present stoc!. :'i!e continuous compoundin(;N:t;< Noe

    !t

    so if !., < &.,@

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    N:t;< Noe!t

    3oublin( Time Approximation

    0or N to be twice No:doublin(;6 e!t< *. %olve for t.Ta!e natural lo( of both sides9

    !t < ln:*; < >.B, so t < ln:*;)!

    #f ! :(rowth rate; is in percent6 you multiply by &>>6 so

    3oublin( time t < B.,)! < >)! :easy to remember9;

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    4The present is the !ey to the past.5

    2rocesses observed now can explain past conditions.

    The present is uniCue because it includes human perturbations

    Dncontrolled experiment with local and (lobal environment.

    We have pushed parts of the system to levels not seen for

    millions of years.

    %- perhaps the past is the !ey to understandin( the future"

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    Eiew that the history of the arth is dominated by sudden

    and sometimes devastatin( events.

    Feolo(ically6 this view su((ests that most of the roc!record preserved bi( events li!e floods or storms6 rather

    than every-day processes.

    nvironmentally6 su((ests that the system is controlled by

    maGor disruptions6 and prone to positive feedbac!s.

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    Stock- The amount of somethin( stored in a 4reservoir5

    Flux- The rate at which somethin( enters or leaves reservoir

    Equilibriumwhen input and output are balanced

    Residence time- stoc!)flux

    Fround water

    +*2eople

    'ehi(h

    Heach sand+onveyor belt

    arths radiation

    Tropical forests

    0ish'obsters?

    /ineral ores

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    Example- Water in a dammed reservoir

    Residence time is volume)outflow

    Time any dissolved pollutants :/TH; remain

    in la!e is environmentally important

    #f pollutant decays faster than residence6 output is clean

    3ama(e limited to :concentrated in; reservoir

    :/ost pollutants 3NT decay9;

    vaporation further concentrates pollutants

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    Linear system-output chan(e is proportional to input chan(e- sprin(

    - twice fertili8er < twice (rowth

    onlinear system-output amplifies or buffers input :feedbac!s;- (laciation

    - ve(etation and rainfall

    !ncertainty- unpredictability of nonlinear systems

    &. Removable co(nitive$ fixed by better measurements6 etc.

    *. #rremediable co(nitive$ cant improve because of nonlinearities

    ,. Eoluntative$ stemmin( from human decision-ma!in(

    :%ee 2iel!e et al. on Hlac!board;

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    0rom physics- the act of observation alters what is bein( observed

    0eedbac! with uncertainty

    Wal! across crowded mall- +annot plan route a priori

    -people chan(e paths in response to your presence

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    arth system contains many nonlinearities and uncertainties.

    "hallen#e$#dentify those aspects that are most sensitive to environmental

    chan(es caused by natural and anthropo(enic activities.

    -3etermine critical thresholds

    -/onitor chan(in( conditions

    -3evelop remediation measures.

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    arth formed I. b.y. a(o - solar nebula

    /aGor events in life correspond to maGor environmental chan(es

    - photosynthesis$oxy(en

    - land plants$less +*- intelli(ence$many disruptions

    cosystem$ +ommunity and its physical environment

    xist at all scales

    Rely on internal interactions between componentsHio(eochemical cycles and ener(y flow

    Hiosphere$ Re(ion where all life exists.

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    1 'ife affects its physical environment

    1 'ife has altered its planetary environment such that it persists

    1 'ife controls the (lobal environment on purpose

    'ife ma!es arth a self re(ulatin( system :7omeostasis;

    -!eeps surface temperature in liCuid water

    -ne(ative feedbac!s

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    3A#%WR'3

    :7omeostatic system;

    % if ! h h i it h d t l

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    9%o if we !now so much6 why is it so hard to solve

    environmental problems?

    &. 2ositive feedbac!s

    *. 'a( time - by the time you see the effect6 it is too late to

    alter the cause. :overshoot and collapse;

    ,. Reversible vs. irreversible impacts

    I. 3iscount rates

    @. 'ow probability6 hi(h impact events

    - meteor

    - maGor volcano6 tsunami6 etc.

    - deadly epidemic

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