Checking up on tropical sunlightJune 11, 2014 in Earth / Earth Sciences
Science is not settled on a bet or a hunch. Measurements and data feed conclusions and provide clarity. Scientists at Pacific Northwest National Laboratory found that two ground-based stations on a tropical island, though less than five miles apart, collect different incoming sunlight measurements based on which way the breezes blow about 10 percent of the time.
The comparison, using data from the Atmospheric Radiation Measurement (ARM) Climate Research Facility Madden-Julian Oscillation (MJO) Investigation Experiment (AMIE) field campaign and the ARM site on Manus Island in Papua New Guinea, confirmed the high quality and representativeness of the measurements taken at the ARM site.
"Our results show that the ground-based measurements at the ARM Manus site are representative of clouds in the region around the site and are less impacted by local island effects than other possible measurement sites on Manus," said Dr. Laura Riihimaki, PNNL atmospheric scientist and lead author of the study. "However, our analysis shows that caution should be used when comparing ground and larger area satellite measurements during easterly wind conditions."
Sunlight energy in, energy out—it's the basis for the Earth's energy budget. Scientists calculate the incoming and outgoing sunlight energy using ground- and satellite-based measurements to better understand how this energy is soaked in by the surface or reflected back into space. When it's cloudy, less of the sunlight energy reaches the Earth's surface. Ground-based measurements are used to test satellite and computer model simulations of the surface energy budget. But, comparing surface irradiance (sun in, sun out) to satellite observations or model simulations can be like comparing apples to oranges. Knowing the difference between the two points of observation, researchers can judge the bias in either set of measurements to better gauge how well each captures the Earth's energy budget over a region or the globe. The information ultimately leads to better understanding of the Earth's climate.
The PNNL team measured the surface irradiance and low cloud base height at a second site on Manus Island in the South Pacific, 7 km (about 5 miles) inland from and slightly more elevated than the standard ARM measurement station at the Momote airport. From these measurements they calculated the impact of clouds (cloud radiative effects, transmissivity, cloud fraction, etc.) using a radiative flux analysis code. They performed statistical comparisons including under different wind conditions and found the greatest differences occur during easterly winds, when the inland site was downwind from the ARM site.
They found the ARM site had more frequent clear skies and a more consistent low cloud fraction under different wind conditions than the site further inland. When the inland site was downwind of the ARM site, there was an increased cloud occurrence, which happened approximately 10 percent of the time.
Under most conditions, the two sites' measurements agreed well: irradiance, cloud amounts, transmissivity, sunshine duration, and frequency of low cloud occurrence. However, they found a greater difference in cloud radiative effects during easterly wind conditions than other times. Further, the Manus site is less impacted by the island meteorology than slightly inland when comparing over a year of broadband surface irradiance and ceilometer measurements, and comparing derived quantities at the standard Manus site and a second location.
The researchers are planning a similar study at the Darwin, Australia, ARM site to examine how representative those measurements are for the wider area.
Riihimaki LD and CN Long. 2014. "Spatial Variability of Surface Irradiance Measurements at the Manus ARM Site." Journal of Geophysical Research: Atmospheres 119(9): 5475-5491. DOI: 10.1002/2013JD021187
Provided by Pacific Northwest National Laboratory
"Checking up on tropical sunlight" June 11, 2014 http://phys.org/news/2014-06-tropical-sunlight.html