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Boundary of advancing mass of warm air
A warm front is a density discontinuity located at the leading edge of a homogeneous warm air mass, and is typically located on the equator-facing edge
Warm_front
Boundary separating two masses of air of different densities
Cold fronts and cold occlusions move faster than warm fronts and warm occlusions because the dense air behind them can lift as well as push the warmer air
Weather_front
Boundary
A pseudo-warm front is a boundary between the in-flow region and the forward-flank downdraft of a supercell. It can either be stationary or move in a northeasterly
Pseudo-warm_front
Meteorological interaction of warm and cool air masses
a warm front near a cyclone, such that the warm air is separated (occluded) from the cyclone center at the surface. The point where the warm front becomes
Occluded_front
Leading edge of a cooler mass of air
A cold front is the leading edge of a cooler mass of air at ground level that replaces a warmer mass of air and lies within a pronounced surface trough
Cold_front
1925 tornado in Missouri, Illinois and Indiana, U.S.
Oklahoma while the warm front shot north into the circulation where the front then extended eastward. A maritime Polar (mP) cold front draped southwestward
1925_Tri-State_tornado
Type of weather map
Cold fronts develop where the cold air mass is advancing, warm fronts where the warm air is advancing, and a stationary front is not moving. Fronts classically
Surface_weather_analysis
Weather front
stationary front may form when a cold or warm front slows down or grows over time from underlying surface temperature differences, like a coastal front. Winds
Stationary_front
Large scale rotating air mass
The cold front over takes the warm front, and reduces the length of the warm front. At this point an occluded front forms where the warm air mass is
Cyclone
Type of middle-altitude cloud
Altostratus clouds usually predict the arrival of warm fronts. Once altostratus clouds associated with a warm front arrive, continuous rain or snow may follow
Altostratus_cloud
Type of cyclone
the poleward portion of the cold front overtakes a section of the warm front, forcing a tongue, or trowal, of warm air aloft. Eventually, the cyclone
Extratropical_cyclone
north as Missouri. This created an anomalously large warm sector–the airmass behind a warm front and ahead of a dry line–for thunderstorms to develop
Tornado outbreak sequence of May 3–11, 2003
Tornado_outbreak_sequence_of_May_3–11,_2003
Characters, formations, and phases of water condensed in the atmosphere
Warm fronts occur where advancing warm air pushes out a previously extant cold air mass. The warm air overrides the cooler air and moves upward. Warm
Precipitation_types
Common type of rain cloud
the SYNOP report. Nimbostratus occurs along a warm front or occluded front where the slowly rising warm air mass creates nimbostratus along with shallower
Nimbostratus_cloud
1925 tornado outbreak in the U.S. states of Missouri, Illinois, and Indiana
throughout the warm sector. The Tri-State supercell formed in a highly favorable area just ahead of the triple point where the cold front, warm front, and dry
1925 Tri-State tornado outbreak
1925_Tri-State_tornado_outbreak
Meteorological model describing the development of cyclones
concept of the warm conveyor belt, which transports warm and moist air just ahead of the cold front above the surface warm front. Polar front theory is attributed
Norwegian_cyclone_model
Clouds with a rippling pattern
Cirrocumulus appears almost exclusively with cirrus some way ahead of a warm front and is a reliable forecaster that the weather is about to change. When
Mackerel_sky
Meteorological term for flow of a fluid into a large collection of itself
inflow focused along their cold front and warm fronts. Tropical cyclones require a large inflow of warmth and moisture from warm oceans in order to develop
Inflow_(meteorology)
Ice storm
April 5, a major low-pressure system crossing Lake Superior pushed a warm front toward eastern Ontario and western Quebec while a high-pressure area over
2023_Canada_ice_storm
Type of cloud
clouds are present. They are formed by warm, moist air being lifted slowly to a very high altitude. When a warm front approaches, cirrostratus clouds become
Stratus_cloud
United States tornado outbreak in May 2025
warm sector. At the surface, a sharpening dryline extended from southeastern Colorado into the eastern Texas Panhandle, while a retreating warm front
Tornado outbreak of May 18–21, 2025
Tornado_outbreak_of_May_18–21,_2025
2024 EF4 tornado in Iowa, U.S.
A warm front extended from the southern low center to the northeast through southeastern Nebraska and over southern Iowa, creating a large warm sector
Greenfield_tornado
District Council, and "Richmondshire" District Council. The Government Warm Front Scheme was re-launched in March 2011 under the UK Coalition Government
Help-Link
Meteorological process of producing weather fronts
fronts. In the end, two types of fronts form: cold fronts and warm fronts. A cold front is a narrow line where temperature decreases rapidly. A warm front
Frontogenesis
Genus of atmospheric cloud
or nitric acid. Cirrostratus clouds sometimes signal the approach of a warm front if they form after cirrus and spread from one area across the sky, and
Cirrostratus_cloud
Genus of mid-level cloud
conjoined altocumulus perlucidus is sometimes found preceding a weakening warm front, where the altostratus is starting to fragment, resulting in patches of
Altocumulus_cloud
Condensed water vapor that falls from clouds
A temperature profile showing a warm layer above the ground is most likely to be found in advance of a warm front during the cold season. Like other
Precipitation
Visible mass of particles suspended in the atmosphere
air is forced aloft at weather fronts and around centers of low pressure by a process called convergence. Warm fronts associated with extratropical cyclones
Cloud
1995 supercell storm in Texas
localized around the distant warm front to the south. Despite the model projections and weather forecasts, the warm front moved north faster than anticipated
1995_Mayfest_Storm
Genus of atmospheric cloud
tropopause. These conditions commonly occur at the leading edge of a warm front. Because absolute humidity is low at such high altitudes, this genus tends
Cirrus_cloud
Cloud species
cumuliform clouds to flatten and become cumulus humilis. In this case, a warm front could be approaching and rain is possible for the next 12 to 24 hours
Cumulus_humilis_cloud
sand. occluded front A type of front formed during the process of cyclogenesis when a cold front overtakes a warm front. Occluded fronts usually form around
Glossary_of_meteorology
Volume of air defined by its temperature and water vapor content
move faster than warm fronts and warm occlusions. Mountains and warm bodies of water can slow the movement of fronts. When a front becomes stationary
Air_mass
37-tornado outbreak in 1975
the warm front, thunderstorms and cloud cover over southern Iowa and northern and central Missouri caused cooler conditions ahead of the warm front, reinforcing
1975_Omaha_tornado_outbreak
Tornado in the United Kingdom
located southwest of Cornwall, with a slow-moving warm front extending across the Midlands and a cold front advancing from the southwest. Early cloud cover
2005_Birmingham_tornado
Precipitation consisting of small, translucent balls of ice
A temperature profile showing a warm layer above the ground is most likely to be found in advance of a warm front during the cold season, but can occasionally
Ice_pellets
1953 tornado in Massachusetts, U.S.
occluded front extended south from it, towards a triple point with a warm front and cold front near the northern end of Lake Superior. The warm front extended
Worcester_tornado
Type of meteorological illustration
cover can help determine whether or not various weather fronts, such as cold fronts or warm fronts, have passed by a location. A nephanalysis, contouring
Station_model
Genus of clouds, low-level cloud
Altocumulus clouds can form via convection or via the forced uplift caused by a warm front. A stratocumulus cloud is another type of stratocumuliform cloud. Like
Cumulus_cloud
Unobstructed view upward from Earth
clouds can lead to halos around the Moon, which indicate the approach of a warm front and its associated rain. Morning fog portends fair conditions and can
Sky
intense precipitation bands in an otherwise stable region, such as in front of a warm front. The same phenomenon is also applicable to oceanography. An air
Conditional symmetric instability
Conditional_symmetric_instability
Development or strengthening of cyclonic circulation in the atmosphere
trailing cold front, and warmer air will push poleward low via the warm front. Usually the cold front will move at a quicker pace than the warm front and "catch
Cyclogenesis
Type of weather boundary
land and the warm offshore currents. The polar front theory says that mid-latitude extratropical cyclones form on boundaries between warm and cold air
Polar_front
States on March 29, 1998. A strong area of low pressure combined with a warm front and favorable upper-level dynamics to produce 16 tornadoes across the
1998 Comfrey–St. Peter tornado outbreak
1998_Comfrey–St._Peter_tornado_outbreak
Windstorms in the southern United States
an initial round of storms and tornadoes associated with the incoming warm front attached to a rapidly deepening low-pressure area over the central Great
Tornado outbreak of March 2–3, 2012
Tornado_outbreak_of_March_2–3,_2012
Form of precipitation
referred to as banded structure. Rainbands in advance of warm occluded fronts and warm fronts are associated with weak upward motion, and tend to be wide
Rain
Water ice in symmetrical shapes
ice crystals. Cirrus clouds are often the sign of an approaching warm front, where warm and moist air rises and freezes into ice crystals. Ice crystals
Ice_crystal
Form of precipitation consisting of rain and melting snow
storm system which sees the wintry mix, as warm air moves northward and above retreating cold air in a warm front, causing snow to change into ice pellets
Rain_and_snow_mixed
Type of cloud
cirrus fibratus occurs at high altitudes. They can indicate an approaching warm front and can also be an indication that fair weather will follow. Fibratus
Cirrus_fibratus
Commuter rail along the Wasatch Front in Utah, United States
From North Temple station, FrontRunner continues northward through Salt Lake City, passing on the northeast side of the Warm Springs Service Center (UTA's
FrontRunner
May 2014 severe weather event in the United States
shear along a warm front enhanced the threat for tornadoes. As the day progressed further, several supercell thunderstorms formed along a front over areas
Tornado outbreak of May 10–12, 2014
Tornado_outbreak_of_May_10–12,_2014
Weather pattern
spring, the front drives cool Atlantic air from the east or northeast into northeastern US that supersedes the warmer continental air. The front is termed
Backdoor_cold_front
Thunderstorm that is characterized by the presence of a mesocyclone
typically found in the warm sector of a low pressure system propagating generally in a north easterly direction in line with the cold front of the low pressure
Supercell
1000-km-order method of measuring weather systems
move faster than warm fronts and warm occlusions. Mountains and warm bodies of water can slow the movement of fronts. When a front becomes stationary
Synoptic_scale_meteorology
Extreme weather event
April 12. This was happening in advance of a slow, northward-progressing warm front. The local atmospheric environment was conducive to heavier precipitation
2023_Fort_Lauderdale_floods
T6 (IF3) tornado in the United Kingdom
18:00 GMT, the leading edge of the storm's precipitation in the form of a warm front had reached Jersey, bringing mainly heavy rain produced by nimbostratus
2023_Jersey_tornado
000 in damage. February 12, 1999 – An unseasonably warm air mass, in conjunction with a cold front, produced a line of thunderstorms that spawned an F1 tornado
List_of_New_Jersey_tornadoes
Methods for describing snowfall events and the resulting snow crystals
associated with intense snowfall. Warm front – Snow may fall as warm air initially over-rides cold in a warm front, circulating around an extratropical
Classifications_of_snow
F5 tornado in 1974
significant moisture advection, destabilization rapidly proceeded apace; the warm front near the Gulf Coast dissipated and then redeveloped northward over the
1974_Brandenburg_tornado
Natural disaster in the US
1:00 p.m. CDT (18:00 UTC). As the warm front bisected central Iowa and stretched into Illinois and Indiana, a cold front and very dry air aloft—indicative
1965 Palm Sunday tornado outbreak
1965_Palm_Sunday_tornado_outbreak
Second-largest tornado outbreak in United States history
significant moisture advection, destabilization rapidly proceeded apace; the warm front near the Gulf Coast dissipated and then redeveloped northward over the
1974_Super_Outbreak
F5 tornado in Ohio and Pennsylvania, U.S.
30, associated with this same cold front (Grazulis, 1990). The day started off on an active note with the warm front moving northwards. A possible tornado
1985_Niles–Wheatland_tornado
1947 windstorm through the U.S. states of Texas, Oklahoma, and Kansas
temperatures ranging from the upper 40s to low 50s °F. However, an approaching warm front—then extended from Sherman, Texas, to Raton, New Mexico—would later combine
Tornado outbreak of April 9–11, 1947
Tornado_outbreak_of_April_9–11,_1947
in Hempfield Township, Pennsylvania. It was rated EF2. On March 29, a warm front over the Gulf of Mexico associated with an upper-level low over Texas
Tornadoes_of_2011
Canada's only F5 tornado
Manitoba throughout the evening. A warm front was positioned north of Elie for much of the day with a trailing cold front residing west of Elie near the Lake
2007_Elie_tornado
−8 °C (28 and 18 °F). Snow may accumulate directly on the trees when a warm front brings wet snow, the air temperature is slightly above the freezing point
Crown_snow-load
Supercell inflow/downdraft boundary
advancing of the downdraft air toward the inflow region. It is a particular form of gust front. National Weather Service Glossary Pseudo-warm front v t e
Pseudo-cold_front
EF4 tornado in 2013
eastern Nebraska. A warm front continued to lift north into northeast Nebraska and western Iowa by late afternoon. With unseasonably warm and moist air in
2013_Wayne_tornado
Atmospheric phenomenon
over a cool surface by advection (wind) and is cooled. It is common as a warm front passes over an area with significant snow-pack. It is most common at sea
Fog
F5 tornado in 1974
significant moisture advection, destabilization rapidly proceeded apace; the warm front near the Gulf Coast dissipated and then redeveloped northward over the
1974_Cincinnati_tornado
Family class 3 cloud type
overcast stratocumulus days, which usually occur either in a warm sector between a warm and cold front in a depression, or in an area of high pressure, in the
Stratocumulus_cloud
Rain maintained at temperatures below freezing
approach of a warm front, when subfreezing air (temperatures at or below freezing) is trapped in the lowest levels of the atmosphere while warm air is advected
Freezing_rain
Natural disaster in the Southeastern US
increased at the surface, contributing to significant warm air advection to the south of a warm front draped across the Appalachian Mountains in North Carolina
1984 Carolinas tornado outbreak
1984_Carolinas_tornado_outbreak
Weather event
Dakota, adjacent to a warm front that extended southeast through southern Minnesota into eastern Iowa. Ahead (north) of the warm front was an area of hot
Western_Wisconsin_Derecho
Genus of high-altitude clouds
these other types of cirrus. This often occurs at the leading edge of a warm front, where many types of cirriform clouds can be present. Cirrocumulus clouds
Cirrocumulus_cloud
Damaging EF3 tornado in Louisiana
Through April 11 and 12, warm air rushed through East Texas, North Louisiana, and Southern Arkansas, associated with a warm front and an upper-level low
2020_Monroe_tornado
Deviation from the normal change of an atmospheric property with altitude
example, a warmer, less-dense air mass moves over a cooler, denser air mass. This type of inversion occurs in the vicinity of warm fronts, and also in
Inversion_(meteorology)
1921 Canadian plan to attack the United States
Peter Carlson (December 30, 2005). "Raiding the Icebox - Behind Its Warm Front, the United States Made Cold Calculations to Subdue Canada". The Washington
Defence_Scheme_No._1
Upcoming survival game
weather patterns of the area; cold and warm fronts form and shift, causing a wide range of weather events, from warm, sunny days to severe tropical storms
Project_Zomboid
Massive 2004 F4 tornado in Nebraska, USA
of the a developing surface low-pressure area, near the dry line and warm front intersection over south-central Nebraska at late noon. Atmospheric soundings
2004_Hallam_tornado
2011 blizzard affecting the U.S. and Canada
Northern and Western Illinois. An ice storm ahead of the winter storm's warm front also brought hazardous conditions to much of the American Midwest and
2011_Groundhog_Day_blizzard
on the afternoon of the June 17, with a warm front stretching across southeastern Minnesota. The warm front combined with pre-existing moisture from
2009_Minnesota_tornadoes
Weather event in the United States
over the Texas and Oklahoma panhandles, with a warm front stretching into northern Louisiana and a cold front stretching along a surface-based trough into
Tornado outbreak sequence of April 2–5, 1957
Tornado_outbreak_sequence_of_April_2–5,_1957
Natural disaster in Switzerland, Austria, Italy and Liechtenstein
Alps: high precipitation due to the meeting of an Atlantic warm front with a polar cold front resulted in 3–4.5 metres of snow being deposited in a two-
Winter_of_Terror
2024 EF3 tornado in Ohio, U.S.
the cold front extending from the low across eastern Kansas into the Texas Hill Country. A large warm sector was expected ahead of the cold front, extending
2024 Lakeview–Russells Point tornado
2024_Lakeview–Russells_Point_tornado
EF4 tornado in Illinois in 2015
late that evening. A cold front stemming from the low progressed eastward across the Mid-South, whereas an arching warm front slowly pushed northward across
2015 Rochelle–Fairdale tornado
2015_Rochelle–Fairdale_tornado
Type of snowstorm
Great Lakes and Midwest. A blizzard also may be formed when a cold front and warm front mix together and a blizzard forms at the border line. Another storm
Blizzard
condensation in buildings which is known as "cold-bridge condensation" or "warm front condensation" where the condensation forms on the interior or exterior
Interstitial_condensation
Tornado Outbreak in April 2002
Nebraska and Iowa, a greater tornado threat was expected to evolve along the warm front and east of the surface low, where wind shear and barometric pressure
Tornado outbreak of April 27–28, 2002
Tornado_outbreak_of_April_27–28,_2002
2007 tornado outbreak in the United States
can be traced back to a powerful, slow-moving low pressure area with a warm front to the north over Nebraska and Missouri. On May 4, the low stalled over
Tornado outbreak of May 4–6, 2007
Tornado_outbreak_of_May_4–6,_2007
Weather event in the United States
of the Appalachian Mountains and extended from Maryland to Georgia. A warm front previously located in the coastal plains had moved into the Piedmont,
1988_Raleigh_tornado_outbreak
Semi-permanent weather front
The Arctic front is the semipermanent, semi-continuous weather front between the cold arctic air mass and the warmer air of the polar cell. It can also
Arctic_front
1839 European windstorm
January, which was replaced on the morning of 6 January by an Atlantic warm front, which brought a period of complete calm with dense, motionless, cloud
Night_of_the_Big_Wind
Storm which affected East Coast of America
December 17th, and being 999 mb by 1205 UTC. The areas north of the system's warm front were the sites of intense convection, and thus hours of heavy rainfall
December_2023_nor'easter
Tornado in 2011
the Ohio Valley during the afternoon and evening. A retreating surface warm front over the region was expected to aid and focus the convection the cluster
2011_St._Louis_tornado
Altitude in which the temperature is at 0 °C
air due to weather fronts. This changes the isotherm gradually, over tens of kilometres for a cold front, and hundreds for a warm front, but the change spreads
Freezing_level
Difference in wind speed or direction over a short distance
surface boundaries with more significant horizontal wind shear than warm fronts. When a front becomes stationary, it can degenerate into a line that separates
Wind_shear
Coating of ice on objects
of rock salt gritting. However, during the early hours of 12 January a warm front moved across the country causing freezing rain and heavy glaze, particularly
Glaze_(ice)
Fur-lined cold weather overgarment
parka is a hip-length cold-weather coat, typically stuffed with down or very warm synthetic fiber, and with a fur-lined hood. The word anorak comes from the
Parka
2019 Tornado event in Alabama and Georgia, United States
the far western Carolinas. An inland stationary front, baroclinic zone and an associated warm front extending southwestward across north-central Georgia
2019_Beauregard_tornado
WARM FRONT
WARM FRONT
Surname or Lastname
English
English : variant spelling of Wharff.
Boy/Male
Muslim
Blossoms, Flowers
Surname or Lastname
English
English : occupational name for a watchman or guard, from Old English weard ‘guard’ (used as both an agent noun and an abstract noun).Irish : reduced form of McWard, an Anglicized form of Gaelic Mac an Bhaird ‘son of the poet’. The surname occurs throughout Ireland, where three different branches of the family are known as professional poets.Surname adopted by bearers of the Jewish surname Warshawski, Warshawsky or some other Jewish name bearing some similarity to the English name.Americanized form of French Guerin.The surname Ward was brought to North America from England independently by several different bearers in the 17th and 18th centuries. Nathaniel Ward (1578–1652), author of the MA legal code, was born in Haverhill, Suffolk, England, and emigrated to Agawam (Ipswich, MA) in 1633. William Ward was one of the original settlers of Sudbury, MA, in about 1638. Miles Ward came from England to Salem, MA, in about 1639. Thomas Ward (d. 1689) settled in Newport, RI, in 1671; among his descendants were two governors of colonial RI.
Male
English
 English occupational surname transferred to forename use, derived from Old English weard, WARD means "guard, watchman."Â
Boy/Male
Norse
Guards the gate of Hell.
Boy/Male
Anglo, British, English, Jamaican
Wise; Watchful; Aware; Watchman; Careful
Boy/Male
Anglo Saxon
Wretched.
Surname or Lastname
English
English : nickname from Old English hearm ‘evil’, ‘hurt’, ‘injury’.English and North German : from a short form of Harman, Hermann.South German : nickname from Middle High German harm ‘ermine’.
Surname or Lastname
English
English : topographic name for someone who lived by a dam or weir on a river (Old English wær, wer), or a habitational name from a place named with this word, such as Ware in Hertfordshire.English : nickname for a cautious person, from Middle English war(e) ‘wary’, ‘prudent’ (Old English (ge)wær).English : Robert Ware came to Dedham, MA, from England in or before 1642. Henry Ware (1764–1845), born in Sherborn, MA, was a Unitarian clergyman and theologian and father of the physician John Ware (b. 1795) and two clergymen, Henry (b. 1794) and William (b. 1797).
Surname or Lastname
German and Danish
German and Danish : variant of Wurm.English : nickname from Middle English wurm ‘serpent’, ‘dragon’ (Old English wyrm).
Boy/Male
Teutonic
warrior.
Boy/Male
Anglo Saxon English
Wise.
Boy/Male
Hindu
Deed, Action
Boy/Male
Shakespearean
King Henry IV, Part 2' Thomas Wart, a country soldier.
Surname or Lastname
English
English : variant spelling of Warne.German : from a short form of any of various Germanic personal names formed with war(in) ‘guard’ as the first element.
Surname or Lastname
English (of Norman origin)
English (of Norman origin) : nickname for a soldier or for a belligerent person, from Old French (de la) werre, (de la) guerre ‘(of the) war’. Compare Delaware.
Boy/Male
Indian
Blossoms, Flowers
Boy/Male
Gujarati, Hindu, Indian, Kannada
Fate; Job; Work
Boy/Male
Teutonic American English Irish
Guard.
Male
German
Short form of German Harman, HARM means "bold/hardy man." In use by the Dutch.
WARM FRONT
WARM FRONT
Girl/Female
Hindu, Indian, Marathi
Unique
Surname or Lastname
English
English : habitational name from any of the various places, for example in Northumbria and North Yorkshire, so named from Old English nÄ“owe ‘new’ + hÄm ‘homestead’.
Surname or Lastname
English
English : variant spelling of Coxon.
Boy/Male
Tamil
Indudar | இநà¯à®¤à¯à®¤à®¾à®°
Boy/Male
Indian, Punjabi, Sikh
Guru
Biblical
those who dwell in villages
Boy/Male
Tamil
Swan
Girl/Female
Australian, British, Christian, English, French, German, Netherlands, Swedish
From Tilden; Matilda; Mighty in War; Battle-mighty; Battle Strength; Powerful in Battle
Boy/Male
Indian, Punjabi, Sikh
Meditation on Lord Unwaveringly
Girl/Female
Tamil
Muktakesha | à®®à¯à®•à¯à®¤à®•ேஷா
One who has open tresses
WARM FRONT
WARM FRONT
WARM FRONT
WARM FRONT
WARM FRONT
a.
Ware; aware.
superl.
Violent; vehement; furious; excited; passionate; as, a warm contest; a warm debate.
v. t.
To make ware or aware; to give previous information to; to give notice to; to notify; to admonish; hence, to notify or summon by authority; as, to warn a town meeting; to warn a tenant to quit a house.
n.
The state of being ware or aware; heed.
v. i.
To collect, and depart from a hive by flight in a body; -- said of bees; as, bees swarm in warm, clear days in summer.
v. i.
To become ardent or animated; as, the speake/ warms as he proceeds.
superl.
Having heat in a moderate degree; not cold as, warm milk.
superl.
Subject to heat; having prevalence of heat, or little or no cold weather; as, the warm climate of Egypt.
v. t.
To ward off.
v. t.
To arrange (yarns) on a warp beam.
a.
A ware; taking notice; hence, wary; cautious; on one's guard. See Beware.
v. i.
To become warm, or moderately heated; as, the earth soon warms in a clear day summer.
a. & n.
A lease of the imposts on particular goods; as, the sugar farm, the silk farm.
v. i.
To wind yarn off bobbins for forming the warp of a web; to wind a warp on a warp beam.
v. t.
To clean by means of a worm; to draw a wad or cartridge from, as a firearm. See Worm, n. 5 (b).
n.
Instruments of war.
v. t.
To make ware; to warn; to take heed of; to beware of; to guard against.
n.
A division of a hospital; as, a fever ward.
a.
To communicate a moderate degree of heat to; to render warm; to supply or furnish heat to; as, a stove warms an apartment.
n.
Anything spiral, vermiculated, or resembling a worm