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ipita tionEarly European Observations°. Precipi aPartitioning byVegetation: A Synthesis anEvaluation of 19th Century FindingsJ80 Friewen Ze And Joh T: Van Stan me: [XPectmient CatchinensHydrojogy, EZ —Meteeshesten

¢“entre fog Envircmenenta Research‘ctmowetetradie

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4* Cortepeecenss Me lheenQuits de. Ted: *49-0341-233. romBs 80 Jay2018, Accept 7 September 2019, Published: 30 September 2049Abstract: Thefirme contact between pre. Pitation and the lane surface is oftenspelling pescipitnts. ”Partitioning bY Vegetation returns water back. to the a

SF intercertus Precipitation)an} iwdistribites water © the subcancpy | —_~

(throughtain Sd water they drains down, Plant stems (temflow), Pric

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Publication Ofthe eid By Horton in 19;9. European Cbeervatories ard a’

beer, Seet¥ing precioitarePartitioningsinc. the mid-19+, century. in thig ——————arlyNMIOLINg ety, OrkS and stisctiog ©Precipitation Partitioning and

OF detail, Nove {9 @ description orth early studies reaults inctucted in th

Uigiticges Andanaly red 'compare them to FOCEN stuctios Although many early

Btatisticn! ALY 806 and Monitoring tools that have becomeStandard today, they“meee ACTly ater, by every BUCY, Of compa) inctuding: 4 Figorous lovel ofdet7 Eterinting Owhich

ig Ofte Lacking in modern Scohydrologicas studies):NRh-resolute

(y throb fat mo aha chonglection 2nd analysis Moreover, é

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My Pieceof history shared by the ty‘drology Metrorolog,, forestry, ang *Bricultural

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10 our synthenig and evaluationMPtion SPOPAlon: through temfow, foreste: crops rain; snow OR: rime

\ dictionMuch OFEarths taySPotheg get Earth Bt shlsce5,for ere by vee tion:

An

betwen Precip St*HHlanie |Lane “plang,coven re se “timated IO ig “OVered byforests |L

teavey throughenon 2nd the lang Surface bs of” 4 pla ditional 115, U1 Thus the fire ContactoPSerato

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dieses Wasser zu trinken. r - (/SS) xs gedacht! erTut er es doch, wird er ~ b>. ee <<\ “\ ) = augenblicklich sterben. \ \ Wo) | —_,_ = uyoo

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|(Asades flyer Proce =) ~~ _ S SSR) =< y {7 | A >Also, all diese dkohydrologischen Prozesse F as@) IG J | . _ SOS Sn a. \

IN wurden vor Jahrhunderten beobachtet. We » 7ich Deg \ a ye— = Aber wann haben die Leute eigentlich tao Gy €,On \ ae Seangefangen sie wirklich zu messen? ye fWiFi, Of, f ~~ ~~,\ pe Op “Op be DEY osmeee id Opp % av > MYene. fi ser m3 “i cape A

( Py Pee é oo aS— i a ef io ee La es TS »)

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ee yy Se ee2s ae’MS ete a aN

Ci Re. | KONIGLICH-SACHSISCHE AKADEMIE FUR FORST-ane — UND LANDWIRTHE ZU THARANDT, DELITSCHLAND,ey es ee 1855PEN 0 i uy eensSekPeal one ‘ ( eae| ARSEaPee eB a Se

fed ¢ &@ ZZ: oo | Hi ois Da AN e y petsyo i “ee.: LY ae - age - J _— imM Fa my ~ ob A ™ a FS 4 ed ©

ak ie 7, 0Ult(“(é‘S y SS ihe te

> a ie) epee Se eraRe Boe Pa pe fires gtSat aN eeo oe a eat en I in ii aa | |! | yi os,a Ax: be Dec* re\y Re <i ~ il 7 rl F oa “ Z A eS j

at Sng Poe een | Sees =)rr | ae of 2 = Sier a / *} -. . y) os Dy. ‘re hk% Fy

yy .' a Ley é

al a >|ES- 7 tT ;, Mein Herr, wir muissenia ; . TT mk ||) guantifizieren wie viel Regen, |a | i. Schnee und Kondensation...

| fla} please on = eaJt AT If [Gye —_ | T <- feahel al in lin > analTELL

i‘ y, bg 2 tatsdchlich den Z , tetb=| Boden erreicht. | ieee9 : |J Ich habe eine Idee!2 —w< - —~AeA s

| KRONENVERDLUNSTLNG NIEDERSCHLAGLi= ie a|waka Pi

KRONENTRAUFE ,

|Tv _‘| STAMMABFLLSS iT || !WALDSTRELIVERDLNSTLNG | o |/ | |i sat |at Krutzschs Idee verbreitete a No.sa __ sich schnell durch ;

die deutschen Konigreiche. + Waldwasserbudget

bs |— Forstlich— | @meteorologische Stationen ° 2)

Viele weitere | ae % rsp §=Europdische Lander | Arsas «=ointeressierten sich at 4a []

auch fur dieses Theme!| AR ae : vm\ i\ 44 ayis ‘g awy eT OS ayAs n>.

yy 4) wai y ona, AL 4 ea |7s . | _— wl ®ye | < — ~ )

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> \ | ei Oa . — 7 Fe if% ~~ .—oe 7 ' = ; x E

| 4-3 an ys y — —. Die ersten Messungen zu ; = — eeStammabfluss verbliifften he Sie fanden auch heraus, aSSwa die Wissenschaftler! p dass sich Verteilungsmuster J 4

/ _ von Regen und Schnee| ae unter Bdumen ... (=

| = eee

" | NViye SAS ota Ia PEN: a Mats an SAR actrees et I to.. hur mit sehr viel mehr Nie) tas ea NGS TRRSMa

___| Messungen erfassen lassen! ~ \ oy SD eae s\ p Cy he tie ah

Cred - il Bee a)ss a ge if fe Dy €%

) Lon

i) +al Lae | a |Y as y |iA Wow! In den Baumkronen y ' /= ff. bleibt ganz schén viel yid| Schnee hangen! re Va

‘ Vj : aN Ly| X / ~ }a y 4 ee Amul a2 SS oeh _—. y

Y .\ Wollny hat sogar viele dieser

// , Prozesse an Feldfrtichten gemessen. (> J y el |7 \ } ) Y ata (

Je ay ae WP|Vf jp KNOY IAL,NY, \ <7 PN, ! ) N

“4 ihry By

aet ‘ 4 pare ; Pe Sat vans os: " TP. oa A e eS on oe 47 . e.oz = “ ae ~ ne oe - a; SS -W* ~~ ,

yy Ds yy y ci a , , “Te y \ , 4 ys 4. a J

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ta? Oe.b airy ¢ i Le Ps ss 3 ee A5 5 oa A | ( / Sead re :.x ee :3

Gx bat | A 6ST 8ayee iT| At es oe S)‘aF Ich frage mich ob sie ihre Ergebnisse geteilt haben? ar SP B; ‘ or ee Das ° a 4 or

L] een ee ve =are INTERNATIONALER VERBAND FORSTLICHER VERSUCHSANSTALTEN,aw,©.Swr 4 — : = cd LyNy ,

a” , :- a se ALT y~ I -w —~ 4 j| p Beeilung Dr. Hoppe! TT) |

Es ist Zeit fur ForstratNeys Vortrag. || | |» a s , Jf, es D| | SS

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ait PAYWelchen Korrekturfaktor +A 51eder59ist kimmert mich nicht. | | rays

age wissen wir nic a = | . |PM cinmalob es 20 oder 80% ist. ah pe ||r|Sid], Sea Py 5= eeBle > oD | lia ,*ai J ,NE o [x ig '—— |i" hire a ah , oy Py 4“=a se ee a4 Le Vk 7 = — | a ~<

an A Sea: am thi> ) | \ ( aC\ Wir haben wichtige Einfltisse wie Holzart,Alter, Klima, Laubausbruch, usw. auBer Achtgelassen. Diese bendtigen weitreichende

und kontinuierliche Messungen und kénnen nurmit Hilfe internationaler Kooperation/ studiert werden,

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Early European Observations of PrecipitationPartitioning by Vegetation: A Synthesis and Evaluationof 19th Century Findingsvon Jan Friesen und John T. van Stan Il

In der SonderausgabeAdvances in Rainfall and Evaporation PartitioningHerausgegeben von Dr. Miriam Coendersund Dr. J.T. van Stan

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