Year-long, broad-band, microwave backscatter observations of an Alpine Meadow over the Tibetan Plateau with a ground-based scatterometer

Abstract

Abstract. A ground-based scatterometer was installed on an alpine meadow over the Tibetan Plateau to study the soil moisture and -temperature dynamics of the top soil layer and air-soil interface during the period August 2017–August 2018. The deployed system measured the amplitude and phase of the ground surface radar return at hourly and half-hourly intervals over 1–10 GHz in the four linear polarization combinations (vv, hh, hv, vh). In this paper we describe the developed scatterometer system, gathered datasets, retrieval method for the backscattering coefficient (σ0), and results of (σ0) for co-polarization. The system was installed on a 5 m high tower and designed using only commercially available components: a Vector Network Analyser (VNA), four coaxial cables, and two dual polarization broadband gain horn antennas at a fixed position and orientation. We provide a detailed description on how to retrieve the co-polarized backscattering coefficients σ0vv & σ0hh for this specific scatterometer design. To account for the particular effects caused by wide antenna radiation patterns (G) at lower frequencies, σ0 was calculated using the narrow-beam approximation combined with a mapping the function G2/R4 over the ground surface. (R is the distance between antennas and the infinitesimal patches of ground surface.) This approach allowed for a proper derivation of footprint positions and -areas, and incidence angle ranges. The frequency averaging technique was used to reduce the effects of fading on the σ0 uncertainty. Absolute calibration of the scatterometer was achieved with measured backscatter from a rectangular metal plate as reference target. In the retrieved time-series of σ0vv & σ0hh for S-band (2.5–3.0 GHz), C-band (4.5–5.0 GHz), and X-band (9.0–10.0 GHz) we observed characteristic changes or features that can be attributed to seasonal or diurnal changes in the soil. For example a fully frozen top soil, diurnal freeze-thaw changes in the top soil, emerging vegetation in spring, and drying of soil. Our preliminary analysis on the collected σ0 time-series data set demonstrates that it contains valuable information on water- and energy exchange directly below the air-soil interface. Information which is difficult to quantify, at that particular position, with in-situ measurements techniques alone. Availability of backscattering data for multiple frequency bands allows for studying scattering effects at different depths within the soil and vegetation canopy during the spring and summer periods. Hence further investigation of this scatterometer data set provides an opportunity to gain new insights in hydro-meteorological processes, such as freezing and thawing, and how these can be monitored with multi-frequency scatterometer observations. The data set is available via https://doi.org/10.17026/dans-zc5-skyg (Hofste and Su, 2020). The effects of fading, calibration, and system stability on the uncertainty in σ0 are estimated to vary from ± 1.3 dB for X-band with vv-polarization to ± 2.7 dB for S-band with hh-polarization through the campaign. The low angular resolution of the antennas result in additional σ0 uncertainty, one that is more difficult to quantify. Estimations point out that it probably will not exceed ± 2 dB with C-band. Despite these uncertainties, we believe that the strength of our approach lies in the capability of measuring σ0 dynamics over a broad frequency range, 1–10 GHz, with high temporal resolution over a full-year period.

Active and Passive Microwave Signatures of Diurnal Soil Freeze-Thaw Transitions on the Tibetan Plateau

“…The ground-based L-band ELBARA-III radiometer and a wide-band scatterometer were installed in a seasonally frozen alpine meadow ecosystem (33.92 • N, 102.16 • E) located in the Maqu County over the northeast Tibetan Plateau [33]- [35]. The elevation of the Maqu site is about 3450 m, and the soil type is sandy loam with an average of 49.7% sand content, 2.2% clay content, and a bulk density of 1 g•cm −3 near the soil surface (i.e., 0-10 cm).…”

“…The antenna boresight angle was fixed at a 55 • angle of incidence, and a computer program was designed to perform the scatterometer's measurements automatically. Recently, the copolarized backscattering coefficients (σ 0 ) at S-(2.5-3.0 GHz), C-(4.5-5.0 GHz), and X-bands (9.0-10.0 GHz) were derived by Hofste et al [33] from the scatterometer measured amplitude and phase of radar return for the period between August 2017 and August 2018.…”

Year-long, broad-band, microwave backscatter observations of an alpine meadow over the Tibetan Plateau with a ground-based scatterometer

“…In the DANS repository, under the link https://doi.org/10.17026/dans-zfb-qegy, the collected scatterometer data are publicly available (Hofste et al, 2021). Stored are both the radar return amplitude and phase for all four linear polarization combinations and processed σ 0 pq for the L-, S-, C-, and X-band bandwidths discussed in this paper.…”

“…This paper describes the scatterometer system and the collected dataset over the period August 2017-August 2018 (Hofste et al, 2021). The radar return amplitude and phase were measured over a broad 1-10 GHz frequency band at all four linear polarization combinations (vv, hv, vh, hh).…”

Multiyear in-situ L-band microwave radiometry of land surface processes on the Tibetan Plateau

“…The time series of LAI is processed with the harmonic analysis of the time series (HANTS) algorithm 26 to remove cloud contaminations. Additional field measurements of fresh and dry above-ground biomass, LAI, and vegetation height were conducted during a field campaign in 2018 27 .…”