Investigating the radiative effect of Arctic cirrus measured in situ during the winter 2015–2016

Abstract

Abstract. The radiative energy budget in the Arctic undergoes a rapid transformation compared with global mean changes. Understanding the role of cirrus clouds in this system is vital, as they interact with short- and long-wave radiation, and the presence of cirrus can be decisive as to a net gain or loss of radiative energy in the polar atmosphere. In an effort to derive the radiative properties of cirrus in a real scenario in this sensitive region, we use in situ measurements of the ice water content (IWC) performed during the Polar Stratosphere in a Changing Climate (POLSTRACC) aircraft campaign in the boreal winter and spring 2015–2016 employing the German High Altitude and Long Range Research Aircraft (HALO). A large dataset of IWC measurements of mostly thin cirrus at high northern latitudes was collected in the upper troposphere and also frequently in the lowermost stratosphere. From this dataset, we select vertical profiles that sampled the complete vertical extent of cirrus cloud layers. These profiles exhibit a vertical IWC structure that will be shown to control the instantaneous radiative effect in both the long and short wavelength regimes in the polar winter. We perform radiative transfer calculations with the uvspec model from the libRadtran software package in a one-dimensional column between the surface and the top of the atmosphere (TOA), using the IWC profiles as well as the state of the atmospheric column at the time of measurement, as given by weather forecast products, as input. In parameter studies, we vary the surface albedo and solar zenith angle in ranges typical of the Arctic region. We find the strongest (positive) radiative forcing up to about 48 W m−2 for cirrus over bright snow, whereas the forcing is mostly weaker and even ambiguous, with a rather symmetric range of values down to -35Wm-2, over the open ocean in winter and spring. The IWC structure over several kilometres in the vertical affects the irradiance at the TOA via the distribution of optical thickness. We show the extent to which IWC profiles with a coarser vertical resolution can reflect this effect. Further, a highly variable heating rate profile within the cloud is found which drives dynamical processes and contributes to the thermal stratification at the tropopause. Our case studies highlight the importance of a detailed resolution of cirrus clouds and the consideration of surface albedo for estimations of the radiative energy budget in the Arctic.

Differences in microphysical properties of cirrus at high and mid-latitudes

“…The lower N observed in HL cirrus compared to ML cirrus is consistent with the observations from Wolf et al (2018). Marsing et al (2023) showed averaged IWCs (0.003 and 0.005 g m −3 ) of two case studies during the POLSTRACC (Polar Stratosphere in a Changing Climate) campaign in line with our measurements at high latitudes.…”

“…In this study we provide new insights into the microphysical properties of the rarely observed Arctic cirrus and support our analysis by backward trajectories of the cirrus air parcels to investigate cirrus formation and evolution. Even though other campaigns have been previously performed in this region (Schiller et al, 2008;Heymsfield et al, 2013;Krämer et al, 2016;Wolf et al, 2018;Marsing et al, 2023), in situ data on the full range of cirrus particle sizes remain limited at high latitudes.…”

Innovative cloud quantification: deep learning classification and finite-sector clustering for ground-based all-sky imaging

“…Generally, clouds absorb a portion of shortwave radiation, scatter another portion and reflect the rest back into space, thereby altering the amount of solar radiation reaching Earth's surface. Cirrus clouds, due to their high altitude and composition of ice crystals, exhibit strong scattering of shortwave radiation and also significantly affect the emission and absorption of longwave radiation (Marsing et al, 2023;Shi and Liu, 2016). Cumulus clouds, with their rough structure, contribute to strong scattering and some degree of absorption of shortwave radiation.…”

Evaluating the Representation of Arctic Cirrus Solar Radiative Effects in the IFS with Airborne Measurements

“…Due to their influence on the radiative energy budget in the Arctic (Marsing et al, 2023), cirrus need to be properly represented in numerical weather prediction (NWP) models. One important component of each NWP model considers the atmospheric radiative transfer, calculating the radiative energy budget and atmospheric heating and cooling rates as a driver for dynamic processes.…”