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slim-4,000 in Wfiflrlama ken,
in large valleys, and especially in eool moisl elimares,
llie upslope wind may resuli in ine general ii a! a
dam ol eiimulus elouds al «be valley liead. rr g oll
as a sueeession bl eluuds lroiri mld—mornlng lo
evening in more rropieal riumid elimaies, ilie eloud
may be eoneinuously end on ine rrioiinrain lops: inis
lonns pan onno sranding eloud ol liigli islands Surn
eloud land rainlalll elleels are aereniuared by loiesl on
me valley sides and ridges. .s uses «11le humidiry
me air slreams by rranspiraiion in nor weallier.
Valleys in rundra and desen suppori lree populalions
absenl lrorn llie plain or peneplain areas surrounding
ibern, bill lne reasons may diller iii rlial rundra valleys
are likely lri be prolesled by ldnyenl deep snow rover
niis preserves warm or sublzlkul soil lemperaruies in
winler las well as pluvlding exress summer men
molslurel Valleys m deserls remain moisl due lo lbe
deep delrirus wnien lills llioir floms', lne shaded soils
lose less moisiure lei evaporaiion Lernal soil
lemperarures are also avoided by paroal shaldmg laoln
lee-blasl and sandeblasi are modilied or absenl in
valley lloors, so inn unproleeled seedlings Ian survive
liign winds m inesnellerolyalleys
'rlius, valleys (or wadisl are prelened growing siles
m deserrs, and provide lree produrls in oilierwise
lreeless lundras, allliougli llie laller sires are rarely
oeeupied by numan selllemenl.
in me lleld, we ollen nonee a sudden eoldness ,usl
belore dawn in valley nus; line is rlie nine ol rne
grealesl deplli ol eold air, and nenee llie greattsl
inlensiry ulwld llrr nowmg down lrorn ilie moimlains
lias pooled all niglil, and yusr belore llie sun rises, we
land many animalsl are or our grearesl exposure and
lowesl elab ii is ai lliis lime rnar - ds oll glaciers
flowing dnwn rald valleys ieaeli llieir maximum speed
Willioui wind or air llow, indiaoon nosr ran lorin, as
n dose in slrelrered liollows and liee Ell-Hugs in lliese
areas, opening up llie elenrmgs or draining lliem oleeild
air may help reduee rrosl, il can is die aim lsigure
5,13)
Wlen, some years ago, i gyew sueli oops as lorriarioes
and eiieurbi ide open lree samples, i did prevenl
lrosl, bul losi crop due lei low liyil levels and a lack ol
wind or irueel pollinalron, in sueli ease, a sliadeside
screen ol ielleelor planrs lacing llie sun would lielp ro
keep liglir Izvels up, and planrs io aroaei bees need lo
be phced around llie eleariiig. Arbnull or ground
browsers vollim loiesrs are also worrisome in gardens
lpeissuin and poreupine lor example). Green-leal
yegerables, bowever, are nol usually ealen, and can be
summarily grown in small lorgl elearings or in open
loresl in lrosry areas
5.3
LATITUDE EFFECTS
Despile llie weak liglil and anon growmg season al
134
nign lsuopolarl lanrudes, me very long summer days
provide rriore llian a sullieienr quanlily ol liglii ior
vigorous plani growiri Tne daily loral lor laie summer
llulyl is «a langleys ar Madras, lnd (will, ban
langleys al Fresno, Calilomia lel, A50 al Fairbanks.
Alnska MN) The average radoiion in lemperare areas
is is lames inalol llie lropies lcnang, 1963!
Thls is accenlualed, on or near cuasis, by ilie
moderale lempemrures noin ilie eonlveerion 0! air over
warm eurrenls in suen areas as Alaska and me
norlnwesr eoaslal regions 0! Europe nie benelil ol
lliose areas is lnar iris generally lower lemperaiiires,
wnieb suil priolosynlliasis. eonler a pnorusynllielie
ellieieney lnal makes a eonsiderable produelion ol
rereal, berries, lumaioes, poisons, and vegerable erirps
loleranl ol anon season/long day mndlnuns nie ollen
deep periglaeial soils provrde rne basis lor irie
produelion ol giganrlr lelrilee, rabbage. spinaelies, and
roor eiopr, so lliai lliese areas are very lavuurable lor
ageloilruie in surnrner,
siieri (nmihnns prevail in Alaska, lreland, Ssolland,
and pans or Norway sneller and added niienenls irrirn
seaweeds and manures yield rirn meadows and heavy
vegerable produeiion during lie long summer days
The small stoneewalled lields ol lreland produce
abundant sweer nay, mm oops, and guns lor siorage
during winier.
Conversely, llie ample liglil al low (equaloriall
lamudes is inellirienl due lo me errremely liigli
lemperalures lliere, and me mess ligni may mean iliai
planls are ligrii saluraled, Pnoiosynlliesis may actually
deeluie in irrelmense lignl, and rise energy buill inlo llie
plants may be less in sunlignl llian in panial sliade.
snade ldown ro a level ol 20% sunliglill is ol greal
benelir in lropieal deserrs and sunny equalorial
ales 'lrials ol sliadeelolli wiili soemli liglil
lransmisrion may greally inerease plani bulk and
produelion, e s ol sugar beer, inus llie imponanoe ol
iree snade and slradeelorli in desens and cleared-area
nopies.
similarly, iemperalures above zsvc (77“F) sliarply
decrease pnolosyninelie ellieieney, so llial llie normal
deserr or Iquimnal eondillon ol nigli liglii and
leniperalure is very inellieienl lor rne produerion ol
planl malei-ial la rue areiie or liigii lariludes, IS'C
lbw: isoyliriiiori foraddpked speeies and eulnvars, and
mind-c lows-in lor uiariy useliil lood planls. Tropies
arenmed [on low piodueiion olrnose erops which can
be also grown in leinperale areas liglil shade may be
the easenrial sompoisenl loir increased yields,
in briglii sunliglil, leal lemperaruies ollen ereeed air
lerriperaiuies, so llial rne dilluse liglil ol ovrreaal or
rloudy days in liigii lariludes lielps planl growslr,
especially aller midday as lemperalures wnuld rlren
also rise above optimum in dlreer sunllglil,
Pbolosynelnelie ellieieney is limiled by line amlity ol
lne leal to oblain rarbein dinxide or by low levels ol
available earbon dioiirde A| nign liglii iniensiry, we
need m supply carbon dioxrde (|o llie saniralion level
ol om. b0 oblain a H limes inerease in pnolosyn-