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MS050
Solar radiation data from benchmark stations at the HJ Andrews Experimental Forest, 1973 to present

CREATOR(S): Mark D Schulze, Christopher Daly, W. Arthur McKee
PRINCIPAL INVESTIGATOR(S): Mark D Schulze, Christopher Daly, Suzanne M. Remillard
ORIGINATOR(S): W. Arthur McKee
OTHER RESEARCHER(S): Mark D Schulze, Sherri L. Johnson, Julia A. Jones, Greg M Cohn, Adam M Kennedy, Stephanie A Schmidt
DATA SET CONTACT PERSON: Adam M Kennedy, Stephanie A Schmidt
ABSTRACTOR: Donald L. Henshaw, Suzanne M. Remillard
METHOD CONTACT: Greg Downing, Greg M Cohn
FORMER INVESTIGATOR: Richard H. Waring, David Greenland, Mark E. Harmon, Don Henshaw, Craig Creel, Frederick A. Bierlmaier, John Moreau, Christoph K Thomas, Michael H. Unsworth, Anne W. Nolin, Adam B. Mazurkiewicz, Alfred B. Levno, Roswell C. Mersereau, Fox Sparky Peterson
METADATA CREATION DATE:
20 Jun 2024
MOST RECENT METADATA REVIEW DATE:
20 Jun 2025
KEYWORDS:
meteorology, climatology, climate change, photosynthetically active radiation, solar radiation, disturbance, monitoring
PURPOSE:
Hydrology, climatology, and biology interact over a wide range of spatial and temporal scales. Continuous interaction among climate, soils, landuse, and vegetation shape the hydrology and ecology of a landscape. Long-term measurements of such variables at various time and space scales provide an essential foundation for understanding ecosystem processes, and document changes in the local, regional, and global environments.
METHODS:
Experimental Design - MS050:
Description:

Much of the early climatological measurements on the Andrews Forest were associated with the investigation of the initial small watersheds experiment (Watersheds 1, 2, 3). The Climatic Station on WS 2 was installed in 1956 to measure precipitation and a hygrothermograph was added in 1958. The High-15 station was established to measure precipitation in 1964 in conjunction with small watersheds 6, 7, 8, and has evolved into a secondary meteorological station. A more general set of modeling needs led to the installation of the Primary Meteorological Station in 1972 to characterize the meso-scale environment. Originally, solar radiation, air temperature, dew point temperature, and windspeed were collected. Along with precipitation from the climatic station on WS 2, these were the primary climatic variables needed for the models predicting the rates at which materials accumulate or move through ecosystems (Waring et al., 1978). Significant improvements to the station were made in 1975, 1979, and 1988, as the station evolved from chart recorders to state-of-the-art digital data loggers (Bierlmaier and McKee, 1989). The Vanilla Leaf Met Station was installed in 1987. The primary intent was to provide micro- meteorological data for a study of seedling survival following clearcut and shelterwood logging at high elevation. Ultimately, the shelterwood site was discontinued and the clearcut site has evolved as a primary high elevation meteorological station.

Four Benchmark Meteorological Stations (BMS) and two second-level stations are included in the MS001 database. The Primary Meteorological and Vanilla Leaf Meteorological BMS are retained. Two new BMS are installed. In 1994, the Upper Lookout Meteorological Station was established at high elevation (4200 ft, ENE aspect) on clearcut L708 in the SE Andrews. In 1995 the Central Meteorological BMS was established at a centrally located site on clearcut L351 (3300 ft, WSW aspect) in the east-central Andrews. A GIS analysis of elevation and aspect indicated the average elevation (3170 ft., 966 m) and average aspect (267 degrees) of the Andrews Forest, and the Central Met Station was located to represent these general averages. Modifications are made to the Primary and Vanilla Leaf Stations to standardize measured variables, temporal resolution, methods, and instrumention across all BMS. Sites will be cleared and required openings maintained following standards of the National Weather Service, the LTER network, and where appropriate, the NADP network. Telemetering of all BMS was completed in 1996. Second-level stations (SLS) at the Hi-15 and WS 2 Climatic Station will continue to be maintained for measurement of precipitation, temperature, and other data to maintain continuity of historical records. These sites also follow established procedural standards.

The BMS include meteorological measurement of air and soil temperature, relative humidity, calculated dew point temperature and vapor pressure deficit, wind speed and direction measurement, incoming solar radiation, photosynthetically active radiation (PAR), soil moisture, snow melt, and snow moisture and depth.

Citation: The Program for Hydroclimatological Measurement at the H.J. Andrews Experimental Forest by Don Henshaw, Arthur McKee, Alok Sikka 18 Aug 1995 http://andrewsforest.oregonstate.edu/research/component/climate/clim95.pdf
Field Methods - MS050: Net radiation:
Description:

View the climate data collection methods used over time at select stations by following the link below. You can filter results by parameter, climate station, and date range, or use the general text search.

https://hjandrews.shinyapps.io/im_methods_history/

Radiation measurements are collected at multiple stations:

PRIMET and VANMET (benchmark stations): NR01 4-component sensors record mean downward and upward shortwave and longwave radiation, plus total net radiation. Data output every 5 minutes starting in 2013.

Daily mean values for all radiation components are post-calculated and reported in watts per m2.

Instrumentation: Net radiation is calculated from components measured by a heated (dewpoint trigger) Hukseflux NR01, 4-component net radiation sensor (upward and downward facing sensors measure both longwave and shortwave solar radiation components and sensor body temperature) with a Campbell Scientific data logger attached to the tower at 600 cm height; values are output every 5 minutes
Field Methods - MS050: Solar PAR:
Description:

View climate data collection methods used by each unique probe by following the links below. Filter results by database code, site code, parameter, probe, climate station, and date range. A general text search is also available.

https://andlter.forestry.oregonstate.edu/MethodCode/View_History.aspx

https://hjandrews.shinyapps.io/im_methods_history/

Photosynthetically Active Radiation (PAR) measurements:

Mean PAR is measured at Central Meteorological Station (CENMET). Output schedule: 5-minute intervals starting April 2015; prior to that, 15-minute intervals starting in 1998.

Maximum solar radiation is based on instantaneous measurements in micromoles per second per square meter. The time of maximum value is accurate to the minute.

Data quality note: Solar radiation sensors commonly read slightly negative at night (-1 to -7 µmol/s/m2). Negative nighttime readings are changed to 0 in the dataset. Because daily averages include these negative values before correction, a minor error exists in the daily values.

Instrumentation: LICOR PAR (photosynthetically active radiation) quantum sensor, Campbell Scientific model LI190SB. The output of the PAR sensor is a daily average, daily maximum and 15 minute averages, and the units are in micromoles/sec/meter2.
Field Methods - MS050: Shortwave radiation:
Description:

View climate data collection methods used over time at select stations by following the link below. Filter results by parameter, climate station, date range, database code, site code, and probe. A general text search is also available.

https://hjandrews.shinyapps.io/im_methods_history/

Solar radiation measurements:

Benchmark stations (PRIMET, CENMET, UPLMET, VANMET): Total incoming solar radiation calculated with 5-minute output starting in 2014 or 2015 (depending on site). Prior to that, 15-minute output starting in 1994.

WS7MET (secondary benchmark site): Pyranometers record mean downward and upward shortwave radiation. Output schedule: 10-minute intervals beginning February 16, 2007; changed to 15 minutes on September 24, 2012; changed to 5 minutes on April 30, 2015. These two pyranometers were removed on September 9, 2022 and replaced with a single upward facing pyranometer (CS320)

PRIMET and VANMET: NR01 net radiometers installed in 2013 to record upward and downward shortwave radiation components.

Data format and units:

Method codes in the dataset differentiate between total incoming and outgoing solar radiation measurements.

Pre-2015 data was output daily in megajoules per m2, along with maximum daily rate of incoming solar radiation (watts per m2) and time of maximum (accurate to the minute). Since 2015, daily mean downward and upward shortwave radiation data are post-calculated and reported in watts per m2.

Historical notes:

Solar radiation measurement at PRIMET began in 1972 with hourly output until 1994. Much of the incoming solar radiation data from the 1970s is estimated. Original data output in langleys has been converted to standard units.

Instrumentation: Kipp and Zonnen solar radiation pyranometer with thermopile type sensor, model CM-6B with Campbell Scientific data logger located on a 1 meter high platform at Primary Met and on top of shelters at other stations. An earlier model used was the CM-5 with an Instrument Interface M4 data logger. Historical method: The signal is recorded continuously from the Lintronic dome solarimeter on a 30-day Rustrak strip chart scaled from 0 to 2.0 cal/cm2/min with a resolution of 0.1 cal/cm2/min. Data loggers used were the Interface Instrument M-2 or M-3. This historical solar sensor was often unreliable. Shortwave incoming solar radiation is measured by a model Campbell Scientific CS320 pyranometer, Campbell Scientific data logger at various height; mean, total solar radiation is output every 5 minutes. Beginning October 1, 2019, total solar radiation is calculated from the 5min mean values using equation: MJ/m2 = val_in_watts * number_seconds_in_period / 1000000'. Prior to that date, total solar radiation was calculated on-logger.
Field Methods - MS050: Longwave radiation:
Description:

View climate data collection methods used over time at select stations by following the link below. Filter results by parameter, climate station, date range, database code, sitecode, and probe. A general text search is also available.

https://hjandrews.shinyapps.io/im_methods_history/

Longwave radiation measurements:

NR01 net radiometers were installed at PRIMET and VANMET benchmark stations in 2013, recording mean upward and downward longwave radiation components. Total longwave radiation measurements began in 2018.

Method codes in the dataset differentiate between mean and total values for incoming and outgoing solar radiation. Since 2015, daily mean downward and upward longwave radiation data are post-calculated and reported in watts per m2.

Instrumentation: Longwave incoming solar radiation is measured by a heated (dewpoint trigger) Hukseflux NR01, 4-component net radiation sensor (upward and downward facing sensors measure both longwave and shortwave solar radiation components and sensor temperature) with a Campbell Scientific data logger attached to the tower at 600 cm height; values are output every 5 minutes (see Method NRT015)
Processing Procedure - MS001: Early PRIMET data :
Description:

A description of the early processing history and instrumentation for the Primary Meteorological Station (PRIMET), 1972-1989, is posted here:

http://andrewsforest.oregonstate.edu/data/studies/ms01/ms001_primet_1972_1989.pdf

Processing Procedures - MS001:
Description: Sensor data streams via WiFi into file servers located at Oregon State University College of Forestry. The files are run through GCE Data Toolbox, which is a comprehensive software framework for metadata-based analysis, quality control, transformation and management of ecological data sets. https://gce-lter.marsci.uga.edu/public/im/tools/data_toolbox.htm. The files are provided on the provisional data page. For processing into final formats, these files are processed through a Python script called Fastbridge where data visualization is possible and QC/QA validation and report logs occur. Data ranges are checked, specific statistical analysis are performed, data are transformed into final FSDB format.
Citation: Sheldon, Wade M. 2002. GCE Data Toolbox for MATLAB. Georgia Coastal Ecosystems LTER, University of Georgia, Athens.
Quality Assurance - Fire effects on data :
Description: The HJ Andrews Experimental Forest was affected by wildfires in 2020, 2023, and, to a lesser degree, 2024. Documentation is being developed that will describe the potential impacts on long-term records, provide the date ranges of direct impact, and describe specific site or data impacts. The use of the BURNED event_code was expanded to include wildfire, and a code was added to each relevant attribute flag to indicate when fire effects are visible in the data (P=Pyro).
SITE DESCRIPTION:
Temperature and rainfall in the Andrews Experimental Forest are are typical of a maritime climate with wet, relatively mild winters and dry, cool summers. Humidity is generally high through winter months, and maximum daily relative humidity approaches 100 percent at night throughout the year. Minimum summer humidities generally hover around 30-50 percent. Temperature extremes range from near 0 degrees F in unusually cold winters to over 100 degrees for brief periods almost every summer. The range in mean annual temperature (1972-2002) is 7.1-10.5 degrees C at a low elevation site (PRIMET). Precipitation varies with elevation - long-term annual average at low elevation (450 m) is 2200 mm, and at high elevation (1200m) is 2600 mm.
TAXONOMIC SYSTEM:
None
GEOGRAPHIC EXTENT:
H. J. Andrews Experimental Forest
ELEVATION_MINIMUM (meters):
436
ELEVATION_MAXIMUM (meters):
1300
MEASUREMENT FREQUENCY:
continuous
PROGRESS DESCRIPTION:
Active
UPDATE FREQUENCY DESCRIPTION:
annually
CURRENTNESS REFERENCE:
Ground condition