l> Cold waiting is dense Return come the black color Rock woodland Student Investigations house Page

Cold waiting is Dense

Introduction:

we wish to set up a learning instance in which students will certainly discover, through the examination and manipulation of actual data indigenous a natural environment, that:air has mass and also density, andcold wait is denser than warm air. These insights space absolutely basic to understanding virtually everything about weather and also climate. Till a student has actually his or she mind firmly roughly these 2 concepts, the or she is not prepared to understand just how storms work, not ready to understand why the prevailing winds blow the method they do, not all set to understand why deserts happen where lock do.Although this two concepts are basic underpinnings of practically every physical process in the atmosphere, they space not intuitively obvious--in fact, they room counter-intuitive. The college student looks about at the waiting skeptically-- if there are so numerous molecules in the air, why can"t we watch them? If air has actually weight, why doesn"t it it is registered on a scale? On hot summer nights, the waiting feels oppressive, heavy--don"t call me that hot August air is low thickness "Air has mass", "air has density", and also "cold air is dense" room the type of statements the students tend to memorize and parrot back, there is no actually transforming their world-view, since these declaration don"t fit v their day-to-day experience of real-life air. Due to the fact that an expertise of the relationship in between density and temperature of wait is fundamental to so countless natural processes, however is counter-intuitive, the is a good investment of student and instructor time to build this understanding upwards indigenous a solid basis in the observation of real data.

Insights/Curriculum Highlights:

Air is made of molecules, and also therefore has mass. Barometric pressure is a measure of exactly how much fixed of air, i.e. How numerous air molecules, exist over the allude of measurement, every the way up come the peak of the atmosphere. Therefore, barometric pressure decreases v elevation. Any given volume of air has density. The density of air deserve to vary from ar to place and from time come time.The distinction in barometric pressure between observation web page at different elevations is a measure of the thickness of waiting in a tower of air in between those two elevations.Cold wait is denser than heat air.

Thinking skills / Pedagogical Highlights:

Making a connection in between laboratory range observations and atmosphere-scale data sets. Drawing on hand-operated observations to explain an aspect of a organic system. Thinking around a phenomenon (density the air) the is invisible. Imagining borders or limits, and also thinking about phenomena in ~ those borders (a shaft of air, a thoreau of air)Linking nature that room detectable come the human senses (e.g. Wait temperature) with molecular scale phenomena (molecules per volume of air).Linking nature that room measurable in ~ the macroscopic range (e.g. Barometric pressure) to molecular range phenomena (number that molecules). Building a chain of reasoning from reason to effect.Building a chain of thinking from observation to interpretation. Utilizing time series graphs; compare how various parameters vary with time. Recognizing that a measurable residential or commercial property varies through time (barometric push rises and falls as weather equipment pass) and additionally through room (barometric pressure decreases with increasing elevation).Recognizing covariance: 2 properties varying in the very same direction under the influence of the same circumstances (barometric press at the open up Lowland website covaries through that at the Ridgetop site). Using a scatterplot; thinking about two or 3 data parameters simultaneously.

Procedure:

1. Introductory hands-on Investigation: do a BarometerStudents create home make barometers and also discuss exactly how they work. Instructions for this task are contained in plenty of middle school science books. See, because that example: R. L. Bonnet and G. D. Keen, earth Science: 49 scientific research Fair Projects, TAB Books, 1990, pp. 127-131.2. Video : Torricelli"s exploration of waiting pressureStudents view and discuss the section of the "Connections" video in which Torricelli"s discovery of air push is illustrated. In this video, a mercury barometer is lugged up a mountainside, and also the mercury is seen to autumn as the climber ascends. (Alternatively, students deserve to read a description of the same exploration in the publication Connections by James Burke, 1978, Little, Brown & Co, Boston, pp. 74-17.) The interpretation is that the weight of the mercury balances the weight of the overlying air. The load of the overlying waiting decreases together the climber rises higher in the atmosphere; for this reason less load of mercury is needed to balance the reduced weight that the overlying air. 3: reproduce Torricelli"s experiment in a tall buildingUsing a handheld barometer, students will measure the barometric push at street level. Then, emulating the experimenter in the "Connections" video, they will climb the stairway or ascend the elevator of a high building, measure up barometric pressure at each landing or at number of stops follow me the way. Lock observe the the air pressure at the street level is greater than at rooftop level (figure 1). Because that a twelve story structure the distinction in air pressure is about 4 mb. The structure needs to it is in at least 8 stories high to register an unambiguous barometric press difference. 4. Data-based investigation: barometric press from BRF Students study barometric push data sets the were tape-recorded at open up Lowland and also Ridgetop sensor sites at black color Rock Forest. (figure 2). Display should it is in zoomed so that a month of 2 at a time is visible. Each pair the students have the right to be responsible for number of months that data. Data can be printed out and scotch recorded together to kind a lengthy time series of a year or much more duration. (If printouts from various students are combined, be sure that every students collection the plot vertical scale the same.) Points to observe:Over time, the barometric pressure at each site goes up and down, up and also down. The periodicity is around a week, however the sample is not really regular.Barometric press at the Ridgetop site is always less 보다 at the open up Lowland site. Barometric press at Ridgetop and also at open Lowland covary: in various other words, once one goes up, the various other goes up; as soon as one goes down, the other goes down. The difference between the barometric pressure at Ridgetop and Open Lowland is larger than the difference between the high and low pressure at one of two people Ridgetop or open up Lowland. In other words, the variability in room is higher than the variability with time in this data set. Point out to figure out and/or discuss: The up and down wiggles of each barometric pressure record reflect weather systems passing across the ar area. (This might be the subject of a separate investigation, in which students discover the relationship between barometer trends and also sunny or rainy weather.) Barometric pressure at the 2 sites covary because they are subject to the very same weather systems.Which site perform you think is at greater elevation? Think around the manual experiment with the hand-held barometer, and around the experimenter in the relationships video. The Ridgetop Site need to be at higher elevation than the open Lowland Site due to the fact that it always has a reduced barometric pressure. Ridgetop has a lower barometric push than open up Lowland due to the fact that fewer molecules of wait lie in between the Ridgetop site and the peak of the atmosphere than lie between the open Lowland site and the height of the atmosphere. We usually think about barometric push variation in the context of changes through time ("the barometer is falling" or "the barometer is rising"), regarded the i of weather systems. Quantitatively, however, the spatial sports of barometric pressure with key is larger than the temporal sport at any kind of given site. (Optional) using your results from the hands-on examination with the barometer and the tall building, plus your observations of barometric pressure at black Rock Forest, calculation the difference in elevation in between the Ridgetop Site and also the open up Lowland Site.5. Data-based investigation: qualitative relationship in between density & temperature that air returning to the long time series of barometric pressure versus time over the food of the year, students will observe the the press difference between the ridgetop and lowland is not constantly exactly the same. The distinction in pressure between the 2 sites is a measure up of the fixed or thickness of the shaft of air in between the lower and higher elevations. What is changing the thickness of the obelisk of air between the ridgetop and lowland elevations? Students examine digital photographs videotaped at the same time and also place every week. Each student or student pair is responsible for one day of data, v data to adjust spaced one or two weeks apart (the entire class should span half a year that data). For their day, each student-pair assembles a paper of paper with the digital photograph, plus a number representing the difference between the barometric press recorded at the ridgetop and also the lowland station on their day (figure 3). The sheets of record will climate be arranged follow me a wall surface in bespeak from lowest to highest number; i.e. In order from least thick to most thick column that air between ridgetop and lowland elevations. The students will certainly then research the photographs, trying to find patterns or trends. We anticipate that the students will certainly observe that the snowy cold-looking photographs room clustered in ~ the high air-density end of the continuum, and also the summery hot- spring photographs room clustered in ~ the short air-density end of the continually (figure 3). Students shot to explain the relationship in between the time the year and also the density of the column of air. Teacher guides discussion with instances of materials that end up being less dense as they obtain warmer, for instance mercury in a barometer. Class eventually hypothesizes that a cold shaft of air is an ext dense 보다 a warm column of wait (figure 4). 6. Data-based investigation: quantitative relationship in between density & temperature of waiting (for strong high school students or undergraduates) Students check the hypothesis (figure 4) the cold air is denser than warmth air, and also that this is why the distinction in barometric pressure in between the Ridgetop and Open Lowland website is larger is cold weather. They make a graph mirroring the air temperature together the elevation variable, and also the difference in between barometric push at open Lowland and Ridgetop as the elevation variable. (figure 5). The distinction in barometric pressure between the open Lowland site and also the Ridgetop site is a measure up of the mass or density of the column of air in between the 2 elevations. Students observe a solid correlation in between temperature and also barometric pressure distinction (figure 5). This supports the hypothesis that waiting temperature is influencing the weight (density) of the pillar of air in between the ridgetop and lowland elevations.


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Teacher can talk about this monitoring in regards to the actions of gas molecule in solution to heating or cooling. Produced by Kim Kastens, Lamont-Doherty planet Observatory (kastens