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Abstract. In coastal polynyas, where sea-ice formation and melting occur, it is crucial to have accurate estimates of heat fluxes in order to predict future sea-ice dynamics. The Amundsen Sea Polynya is a coastal polynya in Antarctica that remains poorly observed by in situ observations because of its remoteness. Consequently, we rely on models and reanalysis that are un-validated against observations to study the effect of atmospheric forcing on polynya dynamics. We use austral summer 2022 shipboard data to understand the turbulent heat flux dynamics in the Amundsen Sea Polynya and evaluate our ability to represent these dynamics in ERA5. We show that cold- and dry-air outbreaks from Antarctica enhance air–sea temperature and humidity gradients, triggering episodic heat loss events. The ocean heat loss is larger along the ice-shelf front, and it is also where the ERA5 turbulent heat flux exhibits the largest biases, underestimating the flux by up to 141 W m−2 due to its coarse resolution. By reconstructing a turbulent heat flux product from ERA5 variables using a nearest-neighbor approach to obtain sea surface temperature, we decrease the bias to 107 W m−2. Using a 1D model, we show that the mean co-located ERA5 heat loss underestimation of 28 W m−2 led to an overestimation of the summer evolution of sea surface temperature (heat content) by +0.76 °C (+8.2×107 J) over 35 d. By obtaining the reconstructed flux, the reduced heat loss bias (12 W m−2) reduced the seasonal bias in sea surface temperature (heat content) to −0.17 °C (−3.30 × 107 J) over the 35 d. This study shows that caution should be applied when retrieving ERA5 turbulent flux along the ice shelves and that a reconstructed flux using ERA5 variables shows better accuracy.
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New calibration procedures for airborne turbulence measurements and accuracy of the methane fluxes during the AirMeth campaigns
Abstract. Low-level flights over tundra wetlands in Alaska and Canada have beenconducted during the Airborne Measurements of Methane Emissions (AirMeth) campaigns to measure turbulent methane fluxesin the atmosphere. In this paper we describe the instrumentation and newcalibration procedures for the essential pressure parameters required forturbulence sensing by aircraft that exploit suitable regular measurementflight legs without the need for dedicated calibration patterns. We estimatethe accuracy of the mean wind and the turbulence measurements. We show thatairborne measurements of turbulent fluxes of methane and carbon dioxide usingcavity ring-down spectroscopy trace gas analysers together with establishedturbulence equipment achieve a relative accuracy similar to that ofmeasurements of sensible heat flux if applied during low-level flights overnatural area sources. The inertial subrange of the trace gas fluctuationscannot be resolved due to insufficient high-frequency precision of theanalyser, but, since this scatter is uncorrelated with the vertical windvelocity, the covariance and thus the flux are reproduced correctly. In thecovariance spectra the -7/3 drop-off in the inertial subrange can bereproduced if sufficient data are available for averaging. For convectiveconditions and flight legs of several tens of kilometres we estimate the fluxdetection limit to be about4 mg m−2 d−1 forw′CH4′‾,1.4 g m−2 d−1 for w′CO2′‾ and4.2 W m−2 for the sensible heat flux.
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- Award ID(s):
- 1724433
- PAR ID:
- 10376509
- Date Published:
- Journal Name:
- Atmospheric Measurement Techniques
- Volume:
- 11
- Issue:
- 7
- ISSN:
- 1867-8548
- Page Range / eLocation ID:
- 4567 to 4581
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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Abstract Vertical energy transports due to dissipating gravity waves in the mesopause region (85–100 km) are analyzed using over 400 h of observational data obtained from a narrow‐band sodium wind‐temperature lidar located at Andes Lidar Observatory (ALO), Cerro Pachón (30.25°S, 70.73°W), Chile. Sensible heat flux is directly estimated using measured temperature and vertical wind; energy flux is estimated from the vertical wavenumber and frequency spectra of temperature perturbations; and enthalpy flux is derived based on its relationship with sensible heat and energy fluxes. Sensible heat flux is mostly downward throughout the region. Enthalpy flux exhibits an annual oscillation with maximum downward transport in July above 90 km. The dominant feature of energy flux is the exponential decrease from 10−2to 10−4 W m−2with the altitude increases from 85 to 100 km and is larger during austral winter. The annual mean thermal diffusivity inferred from enthalpy flux decreases from 303 m2s−1at 85 km to minimum 221 m2s−1at 90 km then increases to 350 m2s−1at 99 km. Results also show that shorter period gravity waves tend to dissipate at higher altitudes and generate more heat transport. The averaged vertical group velocities for high, medium, and low frequency waves are 4.15 m s−1, 1.15 m s−1, and 0.70 m s−1, respectively. Gravity wave heat transport brings significant cooling in the mesopause region at an average cooling rate of 6.7 ± 1.1 K per day.more » « less
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- Free Publicly Accessible Full Text
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Accepted Manuscript1.0
- Journal Article:
- https://doi.org/10.5194/amt-11-4567-2018
