Weather Stations Data [LB]
Restoration site around Upper Lake - Project Stream
on-line at - Weather underground network
on-line at - HOBOlink
Project Stream 2016-Present time Excel file Restoration_2016_12_8.xlsx
Forest Stand on Prospect Hill - Deciduous
Deciduous 2002-2005 Excel-zip file Deciduous_2002-2005.zip
Deciduous 2006-2009 Excel-zip file Deciduous_2006-2009.zip
Deciduous 2010-2015 Excel-zip file Deciduous_2010-2015.zip
Deciduous 2016-Present time Excel file Deciduous_2017_01_10.xlsx
Forest Stand on Prospect Hill - Hemlock
Hemlock 2002-2005 Excel-zip file Hemlock_2002-2005.zip
Hemlock 2006-2009 Excel-zip file Hemlock_2006-2009.zip
Hemlock 2010-2015 Excel-zip file Hemlock_2010-2015.zip
Hemlock 2016-Present time Excel file Hemlock_2017_01_10.xlsx
Field above Ham/McGregor parking lot - Partially Open Field
Open Field 2002-2005 Excel-zip file Open_2002-2005.zip
Open Field 2006-2009 Excel-zip file Open_2006-2009.zip
Open Field 2010-2015 Excel-zip file Open_2010-2015.zip
Open Field 2016-Present time Excel file Open_2017_01_10.xlsx
The roof of the Library - Clapp Lab-Library
Clapp Lab-Library roof 1999-2005 Excel-zip file Clapp-Library_1999-2005.zip
Clapp Lab-Library roof 2006-2010 Excel-zip file Clapp-Library_2006-2010.zip
Clapp Lab-Library roof 2011-2015 Excel-zip file Clapp-Library_2011-2015.zip
Clapp Lab-Library roof 2016-Present time Excel file Clapp-Library_2017_01_10.xlsx
Weather Stations Microclimate Description [PH]
Differences in climate within small geographic areas or even between the top and bottom of a leaf are important to a variety of organisms. For instance, deer on the Mount Holyoke campus use a White Pine stand as a wintering rest and sleep area, because the evergreen cover buffers wind and extremes in daily temperatures. To investigate differences in microclimate due to differences in forest cover, three new weather stations have been installed on the Mount Holyoke campus. These stations are among the stops in the MWCE’s Curricular Trail. All three stations are located on Prospect Hill. The first weather station is in an open field on the North side of Prospect Hill. The second station is in a hemlock stand on the west side of Prospect Hill. The third weather station is near the top of Prospect Hill in a deciduous stand that includes maple, birch and oak trees. In addition to the weather stations described here, Al Werner of the Earth and Environment Department has been running a weather station off of the top of Clapp for several years.
Data from these weather stations are used in both class lab projects and group projects, and by students doing independent or thesis work on campus. We expect to find differences in microclimate due to variations in the ability of various types of vegetation to hold heat and buffer wind. In addition, the Hemlock stand is currently in decline due to an infestation by the Whooly Adelgid. As the Hemlock stand declines, we expect to see changes in the microclimate within that stand.
The weather stations are the Davis Instruments Vantage Pro. They record a variety of parameters including the following- barometric pressure, evapotranspiration, outside humidity, dew point, rainfall (daily, storm, monthly, yearly), rain rate, solar radiation, outside temperature, heat index, UV index, UV dose, wind direction, wind speed, and wind chill.
The stations collect data every ten minutes using a cable that links the Vantage Pro console to the Integrated Sensor Suite (ISS). The ISS unit has the following components: Rain collector, Anemometer vane, Wind cups, UV and solar radiation sensors.
A work-study student downloads the data from the each weather station once a week. She visits each site, removes the debris from the rain collector, and takes the consoles back to the CE where the data is moved from the console to a desktop computer. Once the data is downloaded it is permanently removed from the console. When the console is disconnected from the ISS it continues to collect data as long as the console is within approximately ten meters from the ISS. Each time the console is taken back to the CE, approximately twenty to thirty minutes of data are lost.
Datalogger in the Hemlock stand
HOBO station at the Open site
Explanation of Weather Parameters [LB]
Data range 2002-2010 were collected with the Vantage Pro2 Davis stations.
Data since May, 2010 were collected with HOBO stations.
Davice station parameter description:
Barometric pressure is the pressure exerted on the earth by air in the atmosphere. This is essentially atmospheric pressure, however barometric pressure accounts for the variability in atmospheric pressure that can be attributed to altitude. Barometric pressure is greater in lower altitudes because there is room for air in the atmosphere here than in an alpine environment, for example. In other words, between the Earth and the ceiling of the atmosphere, there is more space for air thus more air pressure where the elevation of the Earth’s surface is lower.
Evapotranspiration is a measurement of the amount of water vapor returned to the air in a given area. Moisture is put into the air from evaporation (the process by which water becomes a vapor suspended in air molecules) and from transpiration (the active exhalation of water through plant skin). This is essentially the opposite of rainfall.
Outside humidity is the amount of water in the air outside of the box in which the console is contained. Relative humidity is an expression of the amount of water held in the air in relation to the amount of water that the air can hold, which is affected by temperature and air pressure. Relative humidity and evapotranspiration are closely related because if the relative humidity is close to its holding capacity, plants’ ability to evapotranspire may be inhibited.
Dew point is the temperature at which air must be cooled for saturation (100% relative humidity) to occur. Dew point can be used to predict minimum overnight temperature and the likelihood of fog, for example. Dew point is an expression of vapor content.
Daily, storm, monthly, yearly rainfall is measured every ten minutes in 0.01in increments.
Solar radiation is a measure of the intensity of the sun’s radiation reaching a horizontal surface. This is an expression of direct radiation and reflected radiation. It is expressed in Watts per square meter.
Outside temperature is measured in degrees Fahrenheit.
Heat index is a measure of how hot or cold it feels. This is affected by the relative humidity and temperature of the outside air and is explained by evapotranspiration. In the summer, for example, it may feel hotter if humidity is high. It feels hotter because evapotranspiration is low. That is, your perspiration that holds your body’s expelled heat does not evaporate as quickly.
UV dose is a measure of the sun’s energy. This energy reaches the Earth as visible, infrared, and ultraviolet rays (UV). The latter may be dangerous to human health. The console measures UV in two forms. The first form Minimum Erythemal Dose (MED) is an index of the relationship between UV exposure and the extent of congestion of small capillaries in skin that redden the skin’s appearance. The MED scale is in whole number units and is presented in relation to a person’s skin type.
The second measurement derived form the UV index is a scale from 1 to 16 that expresses exposure in terms of "likeliness to cause sunburn."
Wind direction is measured using a compass display and Wind speed is measured in miles per hour.
Wind chill is measure of how hot or cold it feels in relation to the temperature and the wind speed. A person’s body releases heat; when it is undisturbed this heat remains near to one’s body affecting one’s perception of the outside temperature. When it is windy this heated air is literally blown away from the body causing one to feel colder. This is measured in a scale related to wind speed (mph).
The depth of soil probes (soil moisture and soil temperature):
#1 = 5 cm
#2 = 20 cm
#3 = 50 cm
Rain gauge - Range: 0-12.7 cm per hour, Resolution: 0.01in. or 0.02 mm, Accuracy: +/-1.0%
PAR sensor - Photosynthetically Acive Radiation - Range: 0-2500µmol/m2/sec or +/-5%, Resolution: 2.5 µmol/m2/sec, Accuracy: <2%. The PAR sensor is designed to detect photons between 400-700 nm in wavelength.
Pyranometer sensor (Solar Radiation) - is designed to measure solar power per unit area (watts per square meter). Ramge: 0-1280 W/m2, Accuracy: +/-5%, +/- 10 w/m2, Resolution: 1.25 W/m2.
Wind Speed/Direction sensor - is designed to measure wind speed, gust and direction. Range: 0-44m/s as a speed and 0-358 degrees as a direction. Accuracy: +/-0.5m/s for the speed and +/-5 degree for the direction. Resolution: 0.19 m/s and 1.4 degree.
Barometric Pressure sensor - is designed to measure the atmospheric pressure. Range: 660-1070 mbar or 19.47-31.55 Hg, Accuracy: +/- 3.0 mbar or 0.088 Hg. Resolution: 0.1 mbar or 0.03 Hg.
Temperature/RH (Relative Humidity) sensor: Range: -40ºC to +75 ºC (-40 ºF to +167 ºF). Accuracy 0.2 ºC. Resolution 0.02 ºC. RH is the amount of moisture in the air compared to what the air can "hold" at that temperature.
Soil Temperature sensor: Range: -40 ºCto +100 ºC (-40 ºF to +212 ºF). Accuracy 0.2 ºC. Resolution 0.03 ºC.
Soil moisture sensor - is designed to measure soil water content. Range:0-0.405 m3/m3. Accuracy: +/-0.041 m3/m3.Resolution: +/-0.0004 m3/m3.
The depth of soil probes (soil moisture and soil temperature):
#1 = 5 cm
#2 = 20 cm
#3 = 60 cm
Page created and maintained by Leszek Bledzki
Peter Houlihan – text and pictures marked [PH]
Leszek A. Bledzki – text and pictures marked [LB]