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MIL-HDBK-850<br />
wading rod-A rod, gmduafad in bat snd<br />
larihs c4 feat, used for @ream gaging in ahaflew<br />
wster.<br />
wall map-A spscisf-purpow map of a targa<br />
ama daaignad IO be dkpfayad on a waff.<br />
w8ndor—Sas zpparant preooaalon.<br />
want of eorreapondcmee-%e y-psraflax.<br />
warpad mocpl-hy spatial rrrodal wtkh, due<br />
to PWOW@UO dielfnthma or wiantdon errors.<br />
haeamodef datunrwhich iadsfermedor<br />
otherwise inaopabls of behg leveled. see also<br />
flat model.<br />
water leveling-A mallwd of obtaining<br />
rale~e abvationa by obaating heights with<br />
rs%=f to the aurtace d a tmdy of stilf wstar.<br />
water atape recordor-An autornstk<br />
r- kwtrumant wirkh rwwrds the ~e *M<br />
tall d the wstar surfacs at s atrasm gaging<br />
station.<br />
wavelength--9 usntilafive apeeifketion of<br />
kinds of radsrd energy. %s ak dominant<br />
Wavolongth.<br />
waving the rod-in leveling, a techn’que<br />
whweby the rodrnan slowty pivots the ksvafhg<br />
rod toward and away fmm Ihs instrument<br />
poaitim The least reading obtainable is the<br />
propar orw to be rwxrrded.<br />
waathar rnap+JCS) A map showing tha<br />
I weather aonditii prsvrding, or predicted 10<br />
I<br />
I<br />
I<br />
Pfma, ovswa sonddersbla araa. Usually, the<br />
rnep is baaed upon westher observations taken<br />
atthaaama Wnestanumberc4 atatkma.AlaO<br />
called ●urfaaa charta; ●ynoptlc chert.<br />
see also map.<br />
waber—(gsomsgneiism) Unit of magnali flux.<br />
In the mks Wstem, 1 weber = 1 pulalamp = 1<br />
kgm2/arrrp .s&.<br />
wedg+optics) A rt#mcting prism of very smsfl<br />
deviation, swh as those used in the eyepieces<br />
of some stemoacopaa. Ataa called 0ptlc8/<br />
wedge.<br />
w<br />
279<br />
weight fasturaa-l%e process of<br />
syatwnslicdly hcmasing the value d IS<br />
padiwlsrdats akwnsr$ ordamantaaoaato<br />
give that akwnanf more aigniticara in the<br />
Snsly.da m .kwtatkme.<br />
walghted mami-A value obtained by<br />
mWW~*da-*d VdUSSbykS<br />
assigned weight and dividing the awn of those<br />
pruducfs by the sum d the waighte.<br />
weight—The ralatiie wIua of an observation,<br />
aourc.a, or qusntity vhwr oorqmmd tih @her<br />
ebservaliona, sources, or qusntdiaa of the aams<br />
or ralatad quanfkii. l-ha Vafua ~fJY<br />
ths most reliable rnsthod is &Qti the<br />
grsatesf weight.<br />
Werner map projectlo~A particufsr caae<br />
of the Bonne map prujectii. in which the<br />
standard psrsllaf is al the pole, end the tangent<br />
cone bamrnaa a tangent pisrw. Any one<br />
geographk rneridiin is cheaen w the centml<br />
meridian and reprasenlad L7ye atrsight &rm,<br />
dwided to axsct scsie. The gsogmphia psrallefs<br />
are raprssamOd bf circular ems, also diviisd 10<br />
exact scale, and the olhsr meridiins are UJrvad<br />
lines.<br />
wast point-see prfma vertiaal plane.<br />
woatlng—See daparture, definitkrn 1.<br />
wide-angla lwt~ lane hsving an angle of<br />
covaraga between 76” end 100”. A bna whose<br />
focsl length is equal to a~roximstaly or#raff<br />
the dmgonal of the format.<br />
wlggflng-fn on firm-..see doubfo<br />
centering.<br />
wlgglJnp-in—A survey proaadura ussd whsn it<br />
is ~ry to astabtish a point, exsdfy am line<br />
befwean two confrvf poinfe nafthar of titi san<br />
be oocupied. If is sssanfialty a tr%d-and-armr<br />
fecfrrriqua where repeated lore end beck<br />
raadinga are taken and the instrument shifted<br />
after each pair of readtrrge until exadfy in tine<br />
with the etaliene. Also called ranging-lrr.<br />
wind rosa-l. A diagram showing the relat”kfe<br />
frsquancy of winds blowing from differsnt<br />
directions. It may also ahow avarsge apssd or