studies have historically relied on observations at towers as a primary source of experimental data on turbulent and mean quantities in the lowest meters of the atmospheric boundary layer.
A large amount of data from numerous flux tower sites, including ET and other micrometeorological
variables, have been collected and archived in global flux network in recent years [8, 9], providing a solid foundation for obtaining helpful knowledge of the underlying mechanisms influencing the variation of ET across various time scales from hourly to interannual.
In the Western United States, NSF-funded researchers deployed a unique set of instruments, called the Internet of Trees Micrometeorological
System, to monitor how trees respond to repeated droughts at the cellular level and across ecosystems.
Griffith DWT, Leuning R, Denmead OT, Jamie IM (2002) Air-land exchanges of C02, CFI4 and [N.sub.2]O measured by FTIR spectrometry and micrometeorological
Thirty-minute averages were calculated for all micrometeorological
measurements and surface water depths for use in further analysis.
Meteorological data were obtained from a micrometeorological
weather station near the experimental area in Argentina as well as in Brazil.
Ishikawa SI, Furukawa A, Oikawa T (1995) Zonal plant distribution and edaphic and micrometeorological
conditions on a coastal sand dune.
On using eco-physiological, micrometeorological
and biochemical theory to evaluate carbon dioxide, water vapour and trace gas fluxes over vegetation: a perspective.
Instrumentation includes soil moisture probes, flumes, suction lysimeters, and micrometeorological
Under Brazilian conditions, vegetable production is based and depends on intensive soil preparation, which alters its physical-hydraulic characteristics and exposes it to wide micrometeorological
variations along the day and along the production cycle (Roman-Paoli et al., 2012; Echer et al., 2014).
features appear to register in the ESP when the descent rate is <2.6 m [s.sup.-1] (taken from the descent rate when the thermal feature was measured in Flt08B).
Sastre et al., "Estimating fog-top height through near-surface micrometeorological
measurements," Atmospheric Research, vol.