<p style="font-weight: 400;"><span>Simultaneous profiling of atmospheric wind and temperature are essential for investigating atmospheric dynamics and wave–mean flow interactions. However, conventional molecular Rayleigh lidar techniques</span>, <span>such as</span><span> hydrostatic integration for temperature retrieval and double-edge discrimination for wind measurement, perform best in aerosol-poor regions and can suffer substantial biases in the troposphere because narrowband Mie scattering contaminates the broadband molecular signal. To overcome this limitation, we developed a high-spectral-resolution lidar (HSRL) receiver based on a Fizeau interferometer and a 32-channel linear photomultiplier-tube array, which spatially resolves the Rayleigh–Brillouin (RB) spectrum across the detector array, allowing Doppler shift and thermally induced spectral broadening to be determined simultaneously and thereby enabling joint wind and temperature retrieval without frequency scanning. Numerical simulations were first performed to optimize the spectral sampling characteristics of the receiver, identifying the 32-channel configuration as a favorable compromise between spectral resolution and signal-to-noise ratio (SNR) over the 2–20 km altitude range. Field measurements were conducted in Urumqi, Xinjiang, China (43.8° N, 87.6° E). Wind profiles were retrieved from 2 to 20 km with a temporal resolution of 10 min, while temperature profiles were independently retrieved from 5.3 to 20 km with a temporal resolution of 5 min. The vertical resolutions were 60 m below 10 km and 300 m above 10 km. Compared with radiosonde measurements, the retrieved temperatures showed mean absolute temperature differences of 1.19 K at 5.3–10 km and 2.10 K above 10 km. Below 5.3 km, wind retrieval used model temperature as an auxiliary input, yielding mean absolute differences of 2.34 and 2.50 m s<sup>−1</sup> for the zonal and meridional wind components, respectively. In the fully lidar-based joint-retrieval region above 5.3 km, the corresponding wind differences were 1.84 and 2.97 m s<sup>−1</sup> at 5.3–10 km and 3.02 and 3.08 m s<sup>−1</sup> above 10 km. These results demonstrate that the proposed scan-free multichannel Fizeau-interferometer HSRL enables reliable temperature profiling from the middle troposphere to the lower stratosphere, while extending wind measurements into the lower troposphere. The proposed receiver provides a compact spectral architecture with potential for future airborne and spaceborne Doppler lidar applications.</span><span></span>