Abstract
Vineyards canopy architecture and row structure pose unique challenges
in modeling the radiation partitioning and energy exchange between the
vine canopy and the interrow area. The vines are often pruned and
manipulated to be strongly clumped while mechanical harvesting requires
wide rows, often with vine height to vine spacing ratio >1. Here we
aimed to estimate the intercepted radiation by the canopy, and the
effect of this interception on the below-canopy surface energy balance
and evapotranspiration (ET). Measurements were conducted in an east-west
oriented vineyard in CA during Intensive Observation Periods (IOPs) as
part of the Grape Remote sensing Atmospheric Profile and
Evapotranspiration eXperiment (GRAPEX). Below-canopy incoming shortwave
radiation was measured at multiple positions across the interrow, and
the surface energy balance/evapotranspiration (ET) below the vine rows
was measured for one growing season using three micro-Bowen ratio (MBR)
systems one in the center of the interrow and one underneath a vine row
south and the other north of the MBR in the center of the interrow. A
significant spatial and temporal variability in radiation was observed
since the vines were not significantly pruned or manipulated so they
were allowed to grow randomly into the interrow. However, when averaged
over the sensor array, the values appeared to give reliable average
radiation extinction conditions that agreed with model estimates. The
variation in the surface energy fluxes were dominated by the amount of
transmitted radiation, while soil moisture was a 2nd order
affect. Daily estimates of ET from the three micro-Bowen ratio systems,
weighted by their respective representative sampling area, yielded
estimates similar to values computed by the correlation-based flux
partitioning method, which utilizes high frequency eddy covariance data.
Original language | English GB |
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State | Published - 1 Dec 2018 |
Externally published | Yes |
Keywords
- 3307 Boundary layer processes
- ATMOSPHERIC PROCESSESDE: 3322 Land/atmosphere interactions
- ATMOSPHERIC PROCESSESDE: 1843 Land/atmosphere interactions
- HYDROLOGYDE: 1866 Soil moisture
- HYDROLOGY