Dew-point.

—Dew is formed whenever falling temperature of the air passes the point where saturation occurs. The reduction of the temperature of air raises the relative humidity because of the diminished capacity to contain moisture. As the temperature declines there will come a point at which the air is saturated and any further decrease of temperature will cause supersaturation. At this point the moisture will be deposited on the cooler surfaces in the form of drops. The temperature at which dew begins to form is known as the dew-point. The sweating of cold water pipes, the dew that forms on a water glass and other relatively cold surfaces is caused by a temperature below the dew-point of the air.

Dew-point Table
Dew-point in degrees Fahrenheit, barometer pressure 29 inches

Air temp.
t
Vapor
press. e
Depression of wet-bulb thermometer (t-)
1.02.03.04.05.06.07.08.0
300.16427252218149+3-5
310.1722926232016115-2
320.1803027242117138+1
330.187312825221915103
340.195322927242016126
350.203333028252218148
360.2113431292623201511
370.2193532302724211713
380.2283633312826231914
390.2373734322927242116
400.2473835333128252218
410.2563937343229262320
420.2664038353330282521
430.2774139363431292623
440.2874240383532302724
450.2984341393634312926
460.3104442403735323027
470.3224543413936343128
480.3344644424037353230
490.3474745434139363431
500.3604846444240373532
510.3734947454341393634
520.3875048464442403735
530.4025149474543413936
540.4175250494744424038
550.4325352504846434139
560.4485453514947454340
570.4655554525048464442
580.4825655535149474543
590.4995756545250484644
600.5175857555351494745
610.5365958565452514946
620.5556059575554525048
630.5756160585655535149
640.5956261595856545250
650.6166362605957555351
660.6386463616058565453
670.6616564626159575654
680.6846765636260585755
690.7076866646361605856
700.7326967666462615957
710.7577068676563626058
720.7837169686665636160
730.8107270696766646261
740.8387371706867656462
750.8667472716968666563
760.8967573727069676664
770.9267674737170686765
780.9577775747271696866
790.9897876757372706967
801.0227977767573727069
Air temp.
t
Vapor
press. e
Depression of wet-bulb thermometer (t-)
9.010.011.012.013.014.015.016.0
300.164-20
310.172-14-50
320.180-9-29
330.187-5-20
340.195-2-14-50
350.203+1-8-28
360.2114-4-19
370.2197-1-12-44
380.2289+3-7-25
390.237126-3-16
400.247148+1-10-35
410.25616114-5-21
420.26617137-1-13-59
430.277191510+3-7-28
440.2872117126-2-17
450.2982219148+2-9-37
460.310242016115-4-20
470.322252218138+0-12-53
480.3342723201510+4-6 -25
490.34728252117137-2 -15
500.36029272319159+2-8
510.3733128252117126-3
520.3873229262319149+1
530.402343128242116115
540.417353229262319148
550.4323634312824211611
560.4483835322926231914
570.4653936343128242116
580.4824038353229262218
590.4994239373431282420
600.5174341383532292622
610.5364442393734312824
620.5554643413835323026
630.5754745424037343128
640.5954846444138363330
650.6164947454340373431
660.6385148464442393633
670.6615250484543403835
680.6845351494744423936
690.7075452508446434138
700.7325553514947454240
710.7575755535149464441
720.7835856545250484543
730.8105957555351494744
740.8386058565453504846
750.8666160585654525047
760.8966261595755535149
770.9266462605856545250
780.9576563615958565452
790.9896664626159575553
801.0226765646260585654

The temperature at which dew forms will depend on the amount of moisture present in the air, but with a definite humidity and air pressure it will always occur at the same temperature. If the dew-point is above freezing, the dew will form as drops of water, but if it is at or slightly below the freezing point, the dew will appear as frost. White frost is formed when the dew-point is only a few degrees below the freezing point. A Black frost occurs when the atmospheric humidity is so low that dew does not form until the temperature is much below the freezing point.