ecological rainfall infrastructure: investment in trees for sustainable development

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Ecological rainfall infrastructure: investment in trees for sustainable development Ecological rainfall infrastructure, Rio Pavillion COP PARIS 02-12-2015 Meine van Noordwijk Chief ScienDst, World Agroforestry Centre (ICRAF); Professor of Agro- forestry, Wageningen University Long cycle: oceans to land Short cycle: Land to land

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Ecologicalrainfallinfrastructure:investmentintreesforsustainabledevelopment

Ecologicalrainfallinfrastructure,RioPavillionCOPPARIS02-12-2015

MeinevanNoordwijkChiefScienDst,WorldAgroforestryCentre(ICRAF);ProfessorofAgro-forestry,WageningenUniversity

Longcycle:oceanstoland

Shortcycle:Landtoland

Forestandwater–bigpictureon‘coolforests’

Q=P-E±ΔS

Streamflow(bluewater):flowpersis-tencedependsonwatershedhealth,asdoeswaterquality

PrecipitaDonof‘rainbowwater’:60%ofrainfalloverlandderivesfromoceans,40%fromvegetaDononland

EvapotranspiraDon(greenwateruse)leadstoaircooling,treesuse100-200mm/yearmorethanshortvegetaDon

Soilwaterstorage(‘spongeeffect’)dependsonsoildepthandstructure

Blue water streamflow

Rainfall triggering conditions

Precipi- tation

Rainbow water Atmospheric transport

Soil & ground-water buffering

Gre

en w

ater

ET

evap

otra

nspi

ratio

n Precipi- tation

Gre

en w

ater

ET

evap

otra

nspi

ratio

n

Blue water streamflow

Soil & ground-water buffering

vanderEntRJ,SavenijeHHG,SchaefliB,Steele-DunneSC,2010.OriginandfateofatmosphericmoistureoverconDnents.WaterResourcesResearch46,W09525,

E/P

PfromEt/P

•  Treesconsumewater•  Treesrecyclewater•  Treeshelpstorewaterbychangingsoiltobe

amoreeffecDvebuffer

•  Streamflowfromhealthycatchmentswithforestsandtreesismoregradual

Higherevapotranspi-raDonmeansmorecoolingeffect

Higherevapotranspi-raDonmeansmoreatmosphericwatervapour

Prevailingwinds

BioDc-pump-inducedairflows?

Oceanicinput

BiologicalprecipitaDontriggers? Rainfall

Downstreamwateruse,livelihoodsrisksandbenefits

Scien1-fic

debate

DownstreamanddownwindbenefitsofwatershedrestoraDon

LightningBNF Denitrifiers

LongcyclerainBRG ET

Stem-flow

Through-fall

Rainfall Cloud interception

Lateral

outflows (interflow) Recharge

Soil surface evaporation

Transpiration

Canopy water evaporation

Uptake

Quick- flow

Base flow

{

Surface run-on Surface

Run-off

Streams & river

Litter layer

Sub-surface lateral inflows

Infil-tra-tion

Percolation

Canopy inter-

ception

CoolingeffectofE

Foresters&farmersmanagingtreecover:ETtranslatedintotree,

cropandpastureproducDvity

NewBRG-science

Rainbowwaterclosesthehydrologicalcycle

Hydrologists:Q,Bluewaterimpliesfocusonstream-flow(floods,drought,useasirrigaDonsource)

Treeecophy-siologists:Et,Greenwaterimpliesfocusonuseofwa-terbyvegeta-Don,compe-DngwithwhatentersstreamsSoilscien1sts:ΔS,Spongeeffectfocusonbufferingbysoilwithgoodinfiltra-Donanddeeprootsystems

Landscapeecologists:scalingfrompatch,viahillslopestowatershedsinrelaDontohumanlanduse

Climatologists:P,PrecipitaDon(rainfall)sourcedfromoceans+land,globalcirculaDon

Decarbonizingthedebateonforests,treesandclimate:cooltrees

Treesmakeitcooler,helpwithrainfallandkeepthesoilmoist

UNFCCC:globalclimatechangedependson

greenhousegasemissions

Thiscarbonthingishardtounderstand,wecan’tseeit…