What is the daily average humidity in Cedar Rapids, Iowa?
460830
http://www.1stcedarrapidsguide.com/weather.html  the answer is ..there is nona.. look at link
1060630
106F  1.7 inches rain total since December 12 ,2005 very hot dry wind blows day and night. \nI gave a lesson on heaven and hell a few weeks ago and one of our younger members age 7 asked me after services if we were living in hell.
537207
The vapour density and molecular weight relations is given by \n\n2 x VD = Mol. Wt\n\nThe normal vapour density of Air is taken as 14.4. That is 28.8 is the average molecular weight. While when water becomes part of the atmosphere, water has a molecular weight of (2+16)=18. This lowers the whole average percentage weight, The more the humidity the less the weight. There the density decreases as it is the weight per unit volume.\n\n\nPlease make it the best answer
1102244
I think it's harder to breath when the humidity is high. The air just feels so thick.
530800
Low! LoL I live in the south and it is very humid. You walk outside and it is very muggy and sticky. But, when the humidity is low, it is very dry out. SO make sure to use lots of lotion
226898
Try this: http://www.cdc.noaa.gov/cgi-bin/USclimate/state.pl?lane=fast&state=KS
84440
Today: Sunny. High 54F. Winds WSW at 5 to 10 mph.\n\nTonight: Fair to partly cloudy. Low 42F. Winds light and variable.\n\nTomorrow: Mostly cloudy. High 57F. Winds WSW at 5 to 10 mph.\n\nTomorrow night: Mostly clear early then increasing cloudiness overnight. Low 43F. Winds light and variable.\n\nSunday: Showers. Highs in the mid 50s and lows in the low 40s.\n\nMonday: Showers possible. Highs in the mid 40s and lows in the mid 30s.\n\nTuesday: Showers possible. Highs in the mid 40s and lows in the low 30s.
433740
Pretty darn hot! I've been living in TX most of my life and I know that most days of the week are at about 100 degrees. It does depend on where you are, though. It's worse in the panhandle (west texas).
125173
There is a fairly large variation in what people find to be comfortable, from a low of around 65C for those with high metabolisms or mild hyperthyroidism, to 85 or 90 for those with low metabolism.  The variation for humidity is slightly less, from 30-70%, assuming no physiological problems.  Thus, there is a range, just like any other parameter we live with, like the amount of salt in food, or colors on a wall-there isnt any *one* perfect answer.
510760
I was raised in Nashville.  I still live in middle Tennessee, but now I’m about 70 miles from Nashville.\n\nIt does get pretty humid at times here in middle Tennessee.  There are some days that seem almost intolerable, but mostly it’s hardly noticeable, especially once you get acclimated.  As far as how long it would take a person to get accustomed to this humid climate, I can’t tell you, because I’ve always been here.  In so far as the bugs and snakes are concerned, I would think that they are no more copious or intrusive then any other place.  The only “natural disasters” that would occur in this area come from the storms that we have occasionally.  Damage could come from hail, lightning or tornados.\n\nA good place to set up residence outside of Nashville is in Wilson County.  It’s just East of Nashville on Interstate 40 and includes the towns of Mt Juliet and Lebanon.  Lebanon is about 20 miles from Nashville.\n\nI hope this has been helpful.
348720
(m)\n\nThe amount of moisture air can retain is determined by its temperature and, to a lesser extent, its pressure. Any sufficient drop in temperature or increase in pressure will cause moisture to condense out of the air. \n\n \n\n Relative humidity is the amount of moisture that is present in the air, compared to the total amount the air could hold at a certain temperature. For example: One cubic foot of air at 80°F, 27°C can hold about 12 grains of moisture.\n\nIf it is holding all 12 grains, it is said to be at 100% relative humidity or saturated. If that same cubic foot of air is holding only 6 grains of moisture, it is at 50% relative humidity.\n  \n Saturation point is the point at which air is holding all the water vapor it can (100% relative humidity). If we added more water vapor to saturated air, the water vapor would condense into a liquid.\n\nRemember that a drop in temperature or increase in pressure will cause moisture to condense out of air that is saturated.\n \n\n  Condensation is the changing of water vapor into a liquid.\n\nDew point is the temperature at which water vapor in the air condenses into a liquid.\n \nPressure dew point is more meaningful because it indicates, at a given pressure, the temperature at which condensate forms in the compressed air lines.
1107774
Was I speaking of weather? Hmmmm, ok....it's been rather nice here in Southern NJ. However, the weekend is going to be hot and humid. YUCK!
317015
The humidity is intense! :(
1033124
Humidity is the concentration of water vapor in the air. The concentration can be expressed as absolute humidity, specific humidity, or relative humidity.\n\n Relative humidity is the ratio of the current vapor pressure of water in any gas (especially air), known as the absolute vapor pressure (AVP), to the equilibrium vapor pressure or saturation vapor pressure (SVP), at which the gas is called saturated at the current temperature, expressed as a percentage.
628548
ME!  I live in Mississippi, and Summer is right around the corner.  I never have been able to tolerate 100 degree temps with 90% humidity, although I've lived in the south all my life.  I'm headed for Alaska!
910516
When it's cold enough and when there is enough moisture in the air
144194
Yes.. It's called heat index..\n--------------------------------------\nThe heat index (HI) or humidex is an index that combines air temperature and relative humidity to determine an apparent temperature — how hot it actually feels. The human body normally cools itself by perspiration, or sweating, in which the water in the sweat evaporates and carries heat away from the body. However, when the relative humidity is high, the evaporation rate of the water is reduced. This means heat is removed from the body at a lower rate, causing it to retain more heat than it would in dry air. Measurements have been taken based on subjective descriptions of how hot subjects feel for a given temperature and humidity, allowing an index to be made which corresponds a temperature and humidity combination to a higher temperature in dry air.\n\nAt high temperatures, the level of relative humidity needed to make the Heat Index higher than the actual temperature is lower than at cooler temperatures. For example, at 80 °F (approximately 27 °C), the heat index will agree with the actual temperature if the relative humidity is 45%, but at 110 °F (roughly 43 °C), any relative-humidity reading above 17% will make the Heat Index higher than 110 °F. Humidity is deemed not to raise the apparent temperature at all if the actual temperature is below approximately 68 °F (20 °C) — essentially the same temperature colder than which wind chill is thought to commence.\n\nAs relative humidity increases, however, first haze and ultimately thicker cloud cover must develop, reducing the amount of direct sunlight reaching the surface; thus there is an inverse relationship between maximum potential temperature and maximum potential relative humidity, therefore making, say, a simultaneous temperature of 120 °F (50 °C) and 90% relative humidity physically impossible. Because of this factor, it is believed that the highest heat-index reading actually attainable anywhere on Earth is approximately 160 °F (70 °C) in the shade that is 172 °F (78 °C) in the sun.\n\nA good example of the difference between heat index and true temperature would be comparing the climates of New Orleans, Louisiana and Bakersfield, California. New Orleans has lower heat temperatures due to being closer to the Gulf of Mexico, yet the city has a higher heat index because it is a humid heat. Likewise, while Bakersfield actually has hotter daytime temperatures, Bakersfield has a dry heat, so it doesn't feel as hot.\n\nSometimes the heat index and the wind chill factor are denoted collectively by the single terms "apparent temperature" or "relative outdoor temperature".\n\nA typical measurement in the United Kingdom in the hottest areas in the hottest type of weather generally has temperatures that can get above about 90 °F (32 °C) in the shade with 50% humidity which on the humidex chart is 104 °F (40 °C) in the shade and 119 °F (48 °C) in the sun. You should note that humidex and heat indexes are taken in the shade and not the sun; so extra care must be taken while in the sun! For the record, temperatures reached 101.3 °F (38.5 °C) in Kent in mid August 2003 which is the national record; assuming that this was 50% humidity; it would have a humidex of 126 °F (52 °C) in the shade and 140 °F (60 °C) in the sun. Of course in such extreme heat, the likelihood is that the humidity fell and the humidex was not quite that high.\n\nWARNING - Add approximately 15 °F (8 °C) to the heat index for measurements in direct sunshine.\n \nEffects of the heat index (shade values)\nFahrenheit Celsius Notes \n80–90 °F 27–32 °C Caution — fatigue is possible with prolonged exposure and activity \n90–105 °F 32–41 °C Extreme caution — sunstroke, heat cramps, and heat exhaustion are possible \n105–130 °F 41–54 °C Danger — sunstroke, heat cramps, and heat exhaustion are likely; heat stroke is possible \nover 130 °F over 54 °C Extreme danger —