North West... during most of hunting season
Sunlight interacting with the Earth's atmosphere makes the sky blue. In outer space the astronauts see blackness because outer space has no atmosphere.
Sunlight consists of light waves of varying wavelengths, each of which is seen as a different color. The minute particles of matter and molecules of air in the atmosphere intercept and scatter the white light of the sun. A larger portion of the blue color in white light is scattered, more so than any other color because the blue wavelengths are the shortest.
When the size of atmospheric particles are smaller than the wavelengths of the colors, selective scattering occurs-the particles only scatter one color and the atmosphere will appear to be that color. Blue wavelengths especially are affected, bouncing off the air particles to become visible.
This is why the sun looks yellow from Earth (yellow equals white minus blue). In space, the sun appears white because there is nothing in between to scatter its white light.
At sunset, the sky changes color because as the sun drops to the horizon, sunlight has more atmosphere to pass through and loses more of its blue wavelengths. The orange and red, having the longer wavelengths and making up more of sunlight at this distance, are most likely to be scattered by the air particles.
The scattering of visible light by atmospheric gases is most correctly called the Tyndall effect, but it is more commonly known to physicists as Rayleigh scattering after Lord Rayleigh, who studied it in more detail a few years later. Rayleigh Scattering is where red, orange, yellow, and green are passed through and blue, indigo, and violet are "scattered" out creating the color.
Whichever direction you look, some of this scattered blue light reaches you. Since you see the blue light from everywhere overhead, the sky looks blue.
(*As for why the sky does not appear violet -- the wavelength most scattered -- see the explanation at the related link below.)
Blue light is scattered in all directions by the tiny molecules of air in Earth's atmosphere. Blue is scattered more than other colors because it travels as shorter, smaller waves. This is why we see a blue sky most of the time.
The sky appears blue to us because of the scattering of the blue light component of the light from the Sun. Some alpine lakes also appear a quite light blue colour for the same reason, light is scattered by tiny suspended flakes of minerals in the water.
Because the water particles in the air split the light and Blue light is dispersed the furthest that's why it creates the illusion the sky is blue
New York has a humid continental climate. Weather in New York is heavily influenced by two continental air masses: a warm, humid one from the southwest and a cold, dry one from the northwest. A cool, humid airflow from the North Atlantic also has an effect on weather in the state, albeit to a lesser extent than the continental ones. Many continental frontal boundaries move across New York, and storm systems moving north along the coast often affect the southern areas of the state.
The winters are long and cold in the Plateau Divisions of the state. In the majority of winter seasons, a temperature of −13 °F (−25 °C) or lower can be expected in the northern highlands (Northern Plateau) and 5 °F (−15 °C) or colder in the southwestern and east-central highlands (Southern Plateau). The Adirondack region records from 35 to 45 days with below zero temperatures in normal to severe winters. Much of Upstate New York, particularly Western and Central New York, are typically affected by lake-effect snows. This usually results in high yearly snowfall totals in these regions. Winters are also long and cold in both Western and Central New York, though not as cold as the Adirondack region. The New York City metro area in comparison to the rest of the state is milder in the winter. Thanks in part to geography (its proximity to the Atlantic and being shielded to the north and west by hillier terrain), the New York metro area usually sees far less snow than the rest of the state. Lake-effect snow rarely affects the New York metro area, except for its extreme northwestern suburbs. Winters also tend to be noticeably shorter here than the rest of the state.
The world's highest recorded air temperature is officially recognized by the World Meteorological Organization as 134°F (57.6°C) recorded at Death Valley, California, USA on 10 July 1913.
Note that this is in recorded history. Higher temperatures have occurred, of course, at different times during the 4.55 billion years of Earth's history.
El Azizia, Libya, held this record for 90 years, after recording a temperature of 136°F (58°C) on 13 September 1922. It was coincidentally also on 13 September of 2012 that this record was stripped by the World Meteorological Organization after a team of experts determined that there were enough questions surrounding this measurement that this temperature probably did not occur.
The temperature had been suspect in atmospheric science circles for a number of reasons. One being that the time of year is inconsistent with such a high reading. Also, the type and exposure of the measuring instruments cast doubt on the accuracy of the data. However, other temperatures in the same general area approach that maximum, especially in the cloudless southern Sahara, far from the moderating effects of water. Several links are provided below for more information on this process.
Other Earth Temperature Highs:
The modern, most reliably recorded air temperature in the world was 129.2°F (54.0°C) at Death Valley on 30 June 2013.
The highest naturally occurring temperature (at Earth's core) is higher than the melting point of iron and is estimated to be approximately 5000°C.
The highest temperature ever created in a laboratory experiment: Scientists, using the Z machine, have produced plasma at temperatures of more than 2 billion degrees Kelvin (3.6 billion degrees F) at Sandia National Laboratories, located near Albuquerque New Mexico.
Dasht-e Lut, a desert in southeastern Iran, was identified as having the hottest surface temperature (not air temperature) of 70.7 degrees C (159 degrees F) This was only during the years of study in 2004 and 2005 by MODIS, which is a satellite remote sensor, mounted on NASA satellites Aqua and Terra.
Caveats to the Above:
Modern measuring methods, instruments, and techniques are more sophisticated and standardized today. Example: The World Meteorological Organization, recommends that air temperatures be measured at a height of 1.25 to 2 meters (which is approximately 4 feet, 1.2 inches to 6 feet, 6.7 inches) above ground level.
The most likely places on Earth for record high temperatures are in depressions in desert regions, especially in areas below sea level. The Dallol (Danakil) Depression in Africa (Ethiopia), Death Valley in USA, and the area around Lake Eyre in Australia are likely candidates. However, the Gobi Desert's temperatures, while far from any ocean, are mitigated by altitude. The Dallol Depression had a weather station for a short while (only a few years). It was run by a mining company, and wasn't there long enough to measure an extreme maximum to beat the Libyan record. It did however, measure very high mean average temperatures while it operated.
The thing to remember about very hot places is that data is sparse. This is because very few people with high levels of technology stay in these places for long. The environment of the Dallol Depression is hostile to human life. 135
The whiteness of the clouds is due to light of all colors being dispersed by the water/ice of the clouds. Clouds quite a distance away appear yellow due to the blue wavelengths being dispered more than the yellow and red wavelengths by the air and particles in the air (the 'clear' sky is blue!)
Not all clouds are pure white, however, for those that are white, it is due to their altitude and the reflection of sunlight.
For example, a cirrus cloud has an altitude of approximately 8km above sea level. At such extreme altitudes all high-level clouds are made up only of ice crystals, as the water vapor from which they are initially formed has frozen.
The ice crystals reflect sunlight. When flying above clouds during the day, they are always bright white. When we get dark clouds, they are so thick that they soak up most of the sunlight or reflect it upwards, and so things aren't as bright below. Storm clouds are the thickest clouds, and look the darkest from down below, though they still look bright white if we see them from above.
Gray color of the clouds is caused by higher clouds casting their shadow on lower-based clouds, or that the clouds are so dense that their top parts absorb most of the sunlight, casting their own shadow along their base, making them dark on the bottom.
WEATHER: Weather is basically the way the atmosphere is behaving, mainly with respect to its effects upon life and human activities. Most people think of weather in terms of temperature, humidity, precipitation, cloudiness, brightness, visibility, wind, and atmospheric pressure, as in high and low pressure. In most places, weather can change from minute-to-minute, hour-to-hour, day-to-day, and season-to-season.
CLIMATE: Climate is the description of the long-term pattern of weather in a particular area.
Some scientists define climate as the average weather for a particular region and time period, usually taken over 30-years. When scientists talk about climate, they're looking at averages of precipitation, temperature, humidity, sunshine, wind velocity, phenomena such as fog, frost, and hail storms, and other measures of the weather that occur over a long period in a particular place.
For example, after looking at rain gauge data, lake and reservoir levels, and satellite data, scientists can tell if during a summer, an area was drier than average. If it continues to be drier than normal over the course of many summers, than it would likely indicate a change in the climate.
In the context of climate change: Weather varies all the time, but climate doesn't vary nearly as quickly.
The Earth's climate is changing relatively quickly (relative to its usual pace) now due to an enhanced greenhouse effect caused by humans emissions of greenhouse gases, and most locations are experiencing a net warming as a result. This doesn't mean it can't get cold anymore, or even that record cold temperatures will no longer occur. But it does mean that, in most areas, heat waves (or unusual warmth in the winter) will be warmer and cold snaps (or cool periods in summer) will not be as cold.
The time scale of climate is not nearly as intuitive as that of weather, so even people who understand this have a tendency to be influenced only by the most recent weather they experience. You can observe this effect by watching the news during both cold snaps and heat waves, which will be either given as evidence for or against the warming of the Earth. In reality, you cannot attribute either to a changing climate due to the small spatial and temporal scale of these events; weather variability will always be of greater magnitude than observed changes in climate.
The instrument, most commonly used in science, is a barometer.
The word, Barometer, is derived from baro, meaning weight or pressure, and meter, meaning measuring device.
Barometers can be either analog or digital. The traditional analog barometer is known as an aneroid barometer. These are the round chrome or brass type that you would normally see on the bridge of a ship, many times accompanied by clock, temperature, and/or humidity gauge.
For an accurate and reliable aneroid barometer, you should expect to pay $249.00 or more. For aneroid barometers, accuracy and reliability will wane incrementally below that price. The cost of scientific instruments, including barometers, are directly tied to accuracy and reliability. In some cases, however, as you go up in price, accuracy will remain stable but quality of materials and craftsmanship will drive the price upwards (i.e. use of thick solid brass or chrome).
Digital barometers emulate the results achieved from an aneroid barometer (sometimes called a "nautical barometer). Their accuracy varies wildly and is not necessarily tied to price. For example, the barometers, in even the most reasonably priced (under $100.00) La Crosse Weather Stations, are exemplary performers. Anecdotal observations over many years show that the La Crosse variance from NIST traceable, accurate weather stations has been minimal (Â±.01). Other inexpensive manufacturer's products have nowhere near this steady and predictable tolerance. And many are as much as .06-.10 or 2-3mb off after initial calibration.
All barometers are not the same. Most have elevation limitations. With the Weems & Plath barometers, specific elevations are designated by each individual product. So, be sure to probe for this information before you buy. Some barometers can be upgraded for high elevation use. But this is relatively expensive, and generally for those barometers to be used in terrain of 5,000ft.
Digital barometers can have the same limitations. Again, be careful when you purchase. We are not aware of any low cost digital that will function correctly over 5,000-6,000 ft elevation. For high altitudes, or if you're a stickler for accuracy, you must consider the Davis, RainWise, WeatherHawk, or Columbia Weather Systems. Do not rely on any barometer above 5,000-6,000 ft for mission critical or safety applications, unless you are absolutely certain of its well defined and guaranteed specifications. Remember that as you begin to challenge the stated limitations of any scientific device, your inaccuracies will almost certainly increase as you approach the stated threshold. For example, a stated 6,000 ft elevation limit may function perfectly well up to 4,000 ft. Then, possibly a gradual fall-off in accuracy between 4,000-5,000ft. But then a rapid and possibly logarithmic increase in error percentage over 5,000ft. This is just an example and not meant to be a basis for calculating decreasing accuracy in any scientific instrument.
The original analog barometer was the water ball. This instrument featured a glass reservoir at its bottom that fed into a narrowing tube that protruded upwards. As atmospheric pressure increased, the water was driven upwards into the tube, to indicate fair or improving weather conditions. Conversely, as the air pressure dropped, the water level in the tube fell, to indicate a change to more inclement weather. As the water level fell even lower in the tube, it became a more urgent indicator of impending foul weather.
Hurricanes and tornadoes are both natural disasters that produce powerful, destructive winds that spiral cyclonically inwards via low pressure (clockwise in the southern hemisphere, counterclockwise in the northern hemisphere).
Hurricanes have a calm, clear eye at the center of rotation and it is believed that many tornadoes have a similar feature.
Both have scales for rating intensity:
Start by multiplying 25 with 9 and divide by 5. Then add 32 to the answer.
In this case the answer is 77 degree Fahrenheit .
The instrument that measures humidity is called a hygrometer.
A hygrometer is an instrument that measures relative humidity in the air. One common kind of hygrometer is a psychrometer, a device that measures the temperature of a wet bulb and a dry bulb simultaneously. The wet bulb should be cooler (if it's above freezing), because water evaporates from the bulb, taking energy with it. If the air is more humid, the evaporation is slower, so the bulb is closer to the dry bulb's temperature. A comparison of the wet and dry bulb temperature using a Psychrometric Chart indicates the relative humidity of the air.
Hygrometers can be combined with other systems as the sensor to regulate humidity. The resulting instrument may be called a humidistat or hygristor, which function somewhat like a thermostat adding or subtracting moisture, not heat, to the air. Types of Hygrometers include:
In term of units; humidity can be expressed by
In term of method, Various equipment can be used to measure water content direct or indirectly.
In term of equipment:
One device is known as a hygrometer. A hygrometer is used to measure humidity.
Not to be confused with the hydrometer which measures the specific gravity of liquids.
A Psychrometer is a type of Hygrometer. A psychrometer consists of two thermometers, one which is dry and one which is kept moist with distilled water on a sock or wick.
As an upgrade in technology there is the trace moisture sensor which is a phosphorous pentoxide (P205), a very hydrophilic material, the resistivity of which changes with the humidity, so it is used in electronic devices designed to make use of the property.
Another tool that could be used is a Cyanometer, an instrument for measuring 'blueness', specifically the color intensity of blue sky. It is attributed to Horace-Bénédict de Saussure and Alexander von Humboldt. It consists of squares of paper dyed in graduated shades of blue and arranged in a color circle or square that can be held up and compared to the color of the sky. The blueness of the atmosphere indicates transparency and the amount of water vapor.
hygrometers and psychrometers
40 °C is equal to 104 °F
The conversion formula is Fahrenheit temperature = (9/5 x Celsius temperature)+ 32
40 degree Celsius = 104 degree Fahrenheit
weather is the daily condition of the atmosphere at a particular time and place.
Atmospheric pressure at sea level is the result of the force of gravity on the matter above sea level (the atmospheric gases). The amount of matter is not constant due to the height and density of the atmosphere (mostly due to temperature and water content/humidity).
Unfortunately for the student, there are many, many different units for measuring atmospheric pressure. Standard air pressure at sea level is most easily defined as 1 atmosphere, or 1 atm.
In terms of an international (ISO) standard, it is defined to be 101325 Pa or 101.3 kPa (kilo-Pascals) at a temperature of 15 Â°C. In meteorology outside of the United States (and sometimes among scientists in the USA), hPa (hectoPascal) is most commonly used (=1013.25 hPa)
Note that a Pascal is also equal to N/m2 - Newtons per square meter, while 1 hpa = 1 mb (millibar) which is convenient for meteorologists, as noted above. Therefore, standard atmospheric pressure also = 1.01325 bar = 1013.25 mb.
The metric value is commonly accepted to be 760mmHg(millimeters of mercury, also "torr"). "Millimeters of Mercury" is a measure that come from a kind of barometer (pressure meter) that uses a column of mercury in a glass tube to measure pressure: The higher the pressure, the taller the column of mercury.
In American units of measure, it's 29.92 in. Hg (inches of mercury) or 14.696 psi (pounds per square inch). This means that, at sea level, the weight of air pressing on every square inch of something is almost 15 pounds.
Something to think about: If you had 1 square inch of room-temperature mercury that was 29.92" tall, it would weigh ... 14.696 pounds!
Again, these are the average atmospheric pressures only at sea level. Pressure drops as we gain altitude; for instance, in Denver, approximately 1 mile above sea level, atmospheric pressure drops to approximately 12.2 PSI or 841.4 millibar.
If you were at sea level, the weight of the air pressing down on you would be 1.03 kilograms per square centimeter.or 1013.25 millibars.
9 upside down is 6. six is smaller than nine.
An anemometer or windmeter is the device that measures wind speed. They are usually divided into those that measure the wind's speed and it's pressure. The first known anemometer was described in 1450 by Leon Battista Alberti.
All forms of water that fall from the clouds are called precipitation. Precipitation includes things like rain, snow, hail and sleet. It is caused when water trapped in the clouds is released due to an inability to keep it floating.
The line where these two air masses meet is called a front.
20°C is equal to 68°F
The conversion formula is °F = (9/5 °C)+ 32
F = [20 * (9/5)] + 32
F = 36 + 32
F = 68.
It's easy to convert from Celsius to Fahrenheit by yourself. Tf = (9/5)*Tc+32, where Tc = temperature in degrees Celsius, Tf = temperature in degrees Fahrenheit.20 C is 68 F.
20 degrees Celsius is 68 degrees Fahrenheit.
Conversion from Celsius to Fahrenheit is done in three steps:
1. Multiply value in degrees Celsius by 9.
2. Divide result of step 1 by 5.
3. Add 32 to result of step 2.
Conversion formula: [°F] = [°C] * 9 / 5 + 32 = 20 * 9 / 5 + 32 = 68 °F
In the United States, the vernal equinox, which signifies the start of astronomical spring in the northern hemisphere, actually happens on March 19, 20, or 21 each year. We haven’t had a March 19 equinox since 1896, and we won’t have a March 21 equinox until 2101.
I say it marks the beginning of astronomical spring because meteorological spring (based on weather patterns) starts March 1.
Astronomical spring is a little harder to explain. The Earth’s axis is always tilted at about 23 degrees, meaning that depending on where it is in its orbit, one hemisphere or the other is closer to the sun. The equinoxes (the vernal equinox in March and the autumnal equinox in September) mark the points in the orbit where neither hemisphere is tilted toward nor away from the sun, meaning day and night are nearly equal.
Start by multiplying 15 with 9 and divide by 5. Then add 32 to the answer.
In this case the answer is 59 degree fahrenheit.
Forest fire is the only big and fairly common natural disaster that afflicts forests.
Cold fronts are defined by cold air advancing, sliding under and displacing warmer air - they are steeper and move more quickly.
Warm air cannot displace cold air easily because it is less dense. Therefore, it rides up and over it, producing stratus and nimbostratus clouds where light precipitation falls.
the boundary of an advancing mass of warm air, in particular the leading edge of the warm sector of a low-pressure system.
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