4.4 Article

A FIRE-ACE/SHEBA Case Study of Mixed-Phase Arctic Boundary Layer Clouds: Entrainment Rate Limitations on Rapid Primary Ice Nucleation Processes

Journal

JOURNAL OF THE ATMOSPHERIC SCIENCES
Volume 69, Issue 1, Pages 365-389

Publisher

AMER METEOROLOGICAL SOC
DOI: 10.1175/JAS-D-11-052.1

Keywords

-

Funding

  1. Office of Science of the U.S. Department of Energy [DE-AC02-05CH11231]
  2. DOE Office of Science, Office of Biological and Environmental Research [DE-AI02-06ER64173, DE-AI02-08ER64547]
  3. NASA
  4. NASA Advanced Supercomputing Division
  5. National Science Foundation
  6. NOAA's Environmental Technology Laboratory
  7. Naval Postgraduate School

Ask authors/readers for more resources

Observations of long-lived mixed-phase Arctic boundary layer clouds on 7 May 1998 during the First International Satellite Cloud Climatology Project (ISCCP) Regional Experiment (FIRE)-Arctic Cloud Experiment (ACE)/Surface Heat Budget of the Arctic Ocean (SHEBA) campaign provide a unique opportunity to test understanding of cloud ice formation. Under the microphysically simple conditions observed (apparently negligible ice aggregation, sublimation, and multiplication), the only expected source of new ice crystals is activation of heterogeneous ice nuclei (IN) and the only sink is sedimentation. Large-eddy simulations with size-resolved microphysics are initialized with IN number concentration N-IN measured above cloud top, but details of IN activation behavior are unknown. If activated rapidly (in deposition, condensation, or immersion modes), as commonly assumed, IN are depleted from the well-mixed boundary layer within minutes. Quasi-equilibrium ice number concentration N-i is then limited to a small fraction of overlying N-IN that is determined by the cloud-top entrainment rate w(e) divided by the number-weighted ice fall speed at the surface upsilon(f). Because w(c) < 1 cm s(-1) and upsilon f > 10 cm s(-1), N-i/N-IN << 1. Such conditions may be common for this cloud type, which has implications for modeling IN diagnostically, interpreting measurements, and quantifying sensitivity to increasing N-IN (when w(e)/upsilon(f) < 1, entrainment rate limitations serve to buffer cloud system response). To reproduce observed ice crystal size distributions and cloud radar reflectivities with rapidly consumed IN in this case, the measured above-cloud N-IN must be multiplied by approximately 30. However, results are sensitive to assumed ice crystal properties not constrained by measurements. In addition, simulations do not reproduce the pronounced mesoscale heterogeneity in radar reflectivity that is observed.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.4
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

Article Meteorology & Atmospheric Sciences

A Machine Learning Correction Model of the Winter Clear-Sky Temperature Bias over the Arctic Sea Ice in Atmospheric Reanalyses

Lorenzo Zampieri, Gabriele Arduini, Marika Holland, Sarah P. E. Keeley, Kristian Mogensen, Matthew D. Shupe, Steffen Tietsche

Summary: This study presents a novel machine learning method to reduce the systematic surface temperature errors in multiple atmospheric reanalyses over sea ice-covered regions of the Arctic under clear-sky conditions. The corrected reanalysis temperature can be utilized to support polar research activities and improve the simulation of the interacting sea ice and ocean system in numerical models.

MONTHLY WEATHER REVIEW (2023)

Article Meteorology & Atmospheric Sciences

Observations of Fog-Aerosol Interactions Over Central Greenland

Heather Guy, Ian M. Brooks, David D. Turner, Christopher J. Cox, Penny M. Rowe, Matthew D. Shupe, Von P. Walden, Ryan R. Neely III

Summary: This study demonstrates that spectrally resolved measurements of downwelling longwave radiation can be used to retrieve the microphysical properties of fogs. In the 12 cases of fog observed in central Greenland, it was found that most of them were mixed-phase fogs, with ice particles having an average effective radius of 24.0 +/- 7.8 μm and liquid droplets having an average effective radius of 14.0 +/- 2.7 μm. The results also support the hypotheses that low aerosol particle concentrations can limit fog liquid water path, fog can increase near-surface aerosol particle concentrations through mixing, and multiple fog events can gradually deplete near-surface aerosol particle concentrations.

JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES (2023)

Article Geosciences, Multidisciplinary

Surface impacts and associated mechanisms of a moisture intrusion into the Arctic observed in mid-April 2020 during MOSAiC

Benjamin Kirbus, Sofie Tiedeck, Andrea Camplani, Jan Chylik, Susanne Crewell, Sandro Dahlke, Kerstin Ebell, Irina Gorodetskaya, Hannes Griesche, Doerthe Handorf, Ines Hoeschel, Melanie Lauer, Roel Neggers, Janna Rueckert, Matthew D. Shupe, Gunnar Spreen, Andreas Walbroel, Manfred Wendisch, Annette Rinke

Summary: Distinct events of warm and moist air intrusions from mid-latitudes have significant impacts on the Arctic climate system. A record-breaking warm air intrusion observed during the MOSAiC expedition in mid-April 2020 is analyzed using Eulerian and Lagrangian frameworks. The intrusion is characterized by two distinct pathways, Siberian and Atlantic, and it has a strong positive effect on the surface energy balance. Model experiments show that moisture availability has a limited impact on the liquid water path in the central Arctic, while increasing cloud condensation nuclei concentrations enhance cloud water content and deepen the atmospheric boundary layer.

FRONTIERS IN EARTH SCIENCE (2023)

Article Multidisciplinary Sciences

The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime

Fange Yue, Helene Angot, Byron Blomquist, Julia Schmale, Clara J. M. Hoppe, Ruibo Lei, Matthew D. Shupe, Liyang Zhan, Jian Ren, Hailong Liu, Ivo Beck, Dean Howard, Tuija Jokinen, Tiia Laurila, Lauriane Quelever, Matthew Boyer, Tuukka Petaja, Stephen Archer, Ludovic Bariteau, Detlev Helmig, Jacques Hueber, Hans-Werner Jacobi, Kevin Posman, Zhouqing Xie

Summary: Based on observations and modeling, it is found that atmospheric mercury in the Arctic is mainly derived from oceanic evasion, particularly in the Marginal Ice Zone (MIZ). This regional process could be the main cause for the summertime peak in mercury concentrations. With rapid Arctic warming and MIZ expansion, oceanic mercury evasion may become more significant.

NATURE COMMUNICATIONS (2023)

Article Multidisciplinary Sciences

Profile observations of the Arctic atmospheric boundary layer with the BELUGA tethered balloon during MOSAiC

Christian Pilz, Michael Lonardi, Ulrike Egerer, Holger Siebert, Andre Ehrlich, Andrew J. Heymsfield, Carl G. Schmitt, Matthew D. Shupe, Birgit Wehner, Manfred Wendisch

Summary: The BELUGA instrument was deployed during the MOSAiC expedition to study the cloudy Arctic atmospheric boundary layer above the sea ice. It collected 66 profile observations, including atmospheric parameters, radiation measurements, aerosol properties, and cloud particle images.

SCIENTIFIC DATA (2023)

Article Multidisciplinary Sciences

Continuous observations of the surface energy budget and meteorology over the Arctic sea ice during MOSAiC

Christopher J. J. Cox, Michael R. R. Gallagher, Matthew D. D. Shupe, P. Ola G. Persson, Amy Solomon, Christopher W. W. Fairall, Thomas Ayers, Byron Blomquist, Ian M. M. Brooks, Dave Costa, Andrey Grachev, Daniel Gottas, Jennifer K. K. Hutchings, Mark Kutchenreiter, Jesse Leach, Sara M. M. Morris, Victor Morris, Jackson Osborn, Sergio Pezoa, Andreas Preusser, Laura D. D. Riihimaki, Taneil Uttal

Summary: The Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) was a yearlong expedition that documented the annual cycle of processes impacting the Arctic atmosphere-ice-ocean system. Measurements of the sea ice's thermodynamic and dynamic evolution were of central importance. This manuscript provides a guide for researchers to access and use the data products acquired during the expedition.

SCIENTIFIC DATA (2023)

Article Meteorology & Atmospheric Sciences

Atmospheric Turbulent Intermittency Over the Arctic Sea-Ice Surface During the MOSAiC Expedition

Changwei Liu, Qinghua Yang, Matthew D. Shupe, Yan Ren, Shijie Peng, Bo Han, Dake Chen

Summary: Turbulent intermittency over the Arctic sea-ice surface was investigated using data collected during the Arctic Climate expedition. The study found that the strength of intermittency increases under specific surface wind speed, wind speed gradient, and air temperature gradient conditions. The analysis also revealed that strong low-level jets favor surface turbulent motions with weak intermittency, while strong temperature inversions above the surface layer lead to strong intermittency.

JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES (2023)

Article Remote Sensing

A cloud detection neural network for above-aircraft clouds using airborne cameras

Joseph Nied, Michael Jones, Shane Seaman, Taylor Shingler, Johnathan Hair, Brian Cairns, David Van Gilst, Anthony Bucholtz, Sebastian Schmidt, Seethala Chellappan, Paquita Zuidema, Bastiaan Van Diedenhoven, Armin Sorooshian, Snorre Stamnes

Summary: We developed a camera-based cloud detection method using a convolutional neural network, which accurately detects clouds above the aircraft and can be used for airborne passive remote sensing. By using human-labeled validation data, we demonstrated the high accuracy of this method in cloud detection. We also compared the performance of this method with traditional zenith cameras for cloud detection instruments, showing that it provides a cost-effective solution for cloud detection in airborne science research flights.

FRONTIERS IN REMOTE SENSING (2023)

Article Geosciences, Multidisciplinary

Spatially coordinated airborne data and complementary products for aerosol,gas, cloud, and meteorological studies: the NASA ACTIVATE dataset

Armin Sorooshian, Mikhail D. Alexandrov, Adam D. Bell, Ryan Bennett, Grace Betito, Sharon P. Burton, Megan E. Buzanowicz, Brian Cairns, Eduard V. Chemyakin, Gao Chen, Yonghoon Choi, Brian L. Collister, Anthony L. Cook, Andrea F. Corral, Ewan C. Crosbie, Bastiaan van Diedenhoven, Joshua P. DiGangi, Glenn S. Diskin, Sanja Dmitrovic, Eva-Lou Edwards, Marta A. Fenn, Richard A. Ferrare, David van Gilst, Johnathan W. Hair, David B. Harper, Miguel Ricardo A. Hilario, Chris A. Hostetler, Nathan Jester, Michael Jones, Simon Kirschler, Mary M. Kleb, John M. Kusterer, Sean Leavor, Joseph W. Lee, Hongyu Liu, Kayla McCauley, Richard H. Moore, Joseph Nied, Anthony Notari, John B. Nowak, David Painemal, Kasey E. Phillips, Claire E. Robinson, Amy Jo Scarino, Joseph S. Schlosser, Shane T. Seaman, Chellappan Seethala, Taylor J. Shingler, Michael A. Shook, Kenneth A. Sinclair, William L. Smith Jr, Douglas A. Spangenberg, Snorre A. Stamnes, Kenneth L. Thornhill, Christiane Voigt, Holger Voemel, Andrzej P. Wasilewski, Hailong Wang, Edward L. Winstead, Kira Zeider, Xubin Zeng, Bo Zhang, Luke D. Ziemba, Paquita Zuidema

Summary: The ACTIVATE experiment by NASA produced a unique dataset for studying aerosol-cloud-meteorology interactions. It used two aircraft to conduct coordinated flights over the northwest Atlantic Ocean, resulting in a comprehensive dataset covering different seasons. The data from both aircraft help to characterize the vertical column of the atmosphere.

EARTH SYSTEM SCIENCE DATA (2023)

Article Environmental Sciences

Warm air intrusions reaching the MOSAiC expedition in April 2020-The YOPP targeted observing period (TOP)

Gunilla Svensson, Sonja Murto, Matthew D. Shupe, Felix Pithan, Linus Magnusson, Jonathan J. Day, James D. Doyle, Ian A. Renfrew, Thomas Spengler, Timo Vihma

Summary: During the MOSAiC expedition in the spring period, efforts were made to increase the radiosounding frequency to study warm air intrusions in the Arctic. Two episodes of increased surface temperatures were observed during a targeted observing period. The circulation patterns guided the warm air into the Arctic region through three different transport pathways. The study showed discrepancies between MOSAiC observations and ERA5 reanalysis in representing small-scale processes, highlighting the need for improvement in numerical weather prediction and climate models.

ELEMENTA-SCIENCE OF THE ANTHROPOCENE (2023)

Article Environmental Sciences

The characteristics of atmospheric boundary layer height over the Arctic Ocean during MOSAiC

Shijie Peng, Qinghua Yang, Matthew D. Shupe, Xingya Xi, Bo Han, Dake Chen, Sandro Dahlke, Changwei Liu

Summary: By analyzing the dataset, we improved the algorithm and studied the characteristics and variability of the atmospheric boundary layer height (ABLH) in the Arctic region. The annual variation of ABLH is primarily controlled by the evolution of ABL thermal structure. Meteorological and turbulence variables also play a significant role in ABLH variation. In addition, the ABLH during the MOSAiC expedition is more suppressed than during the SHEBA experiment in the summer, indicating large variability in the Arctic ABL structure.

ATMOSPHERIC CHEMISTRY AND PHYSICS (2023)

Article Environmental Sciences

On the differences in the vertical distribution of modeled aerosol opticaldepth over the southeastern Atlantic

Ian Chang, Lan Gao, Connor J. Flynn, Yohei Shinozuka, Sarah J. Doherty, Michael S. Diamond, Karla M. Longo, Gonzalo A. Ferrada, Gregory R. Carmichael, Patricia Castellanos, Arlindo M. da Silva, Pablo E. Saide, Calvin Howes, Zhixin Xue, Marc Mallet, Ravi Govindaraju, Qiaoqiao Wang, Yafang Cheng, Yan Feng, Sharon P. Burton, Richard A. Ferrare, Samuel E. LeBlanc, Meloe S. Kacenelenbogen, Kristina Pistone, Michal Segal-Rozenhaimer, Kerry G. Meyer, Ju-Mee Ryoo, Leonhard Pfister, Adeyemi A. Adebiyi, Robert Wood, Paquita Zuidema, Sundar A. Christopher, Jens Redemann

Summary: The study reveals significant differences in estimates of regional aerosol radiative effects over the southeastern Atlantic and emphasizes the need to improve the accuracy of modeled aerosol distributions. Current Earth system models do not fully account for the upper parts of decoupled boundary layers, leading to limitations in simulating low-level clouds. These differences impact the net aerosol radiative forcing, particularly when aerosols interact with clouds.

ATMOSPHERIC CHEMISTRY AND PHYSICS (2023)

Article Environmental Sciences

An attribution of the low single-scattering albedo of biomass burning aerosol over the southeastern Atlantic

Amie Dobracki, Paquita Zuidema, Steven G. Howell, Pablo Saide, Steffen Freitag, Allison C. Aiken, Sharon P. Burton, Arthur J. Sedlacek III, Jens Redemann, Robert Wood

Summary: Aerosol over the remote southeastern Atlantic is highly sunlight-absorbing and its properties are influenced by black carbon (BC) content and combustion efficiency. The aerosols are primarily emitted from grass fires in the miombo woodlands of Angola. The age and transport of the aerosols result in variations in particle size, BC content, and organic aerosol (OA) to BC mass ratios.

ATMOSPHERIC CHEMISTRY AND PHYSICS (2023)

Article Meteorology & Atmospheric Sciences

The CHROMA cloud-top pressure retrieval algorithm for the Plankton, Aerosol, Cloud, ocean Ecosystem (PACE) satellite mission

Andrew M. M. Sayer, Luca Lelli, Brian Cairns, Bastiaan van Diedenhoven, Amir Ibrahim, Kirk D. Knobelspiesse, Sergey Korkin, P. Jeremy Werdell

Summary: This paper provides the theoretical basis and simulated retrievals for the Cloud Height Retrieval from O-2 Molecular Absorption (CHROMA) algorithm. Simulations for OCI and OLCI demonstrate that CHROMA can meet the CTP error goal for PACE mission. CHROMA also provides pixel-level uncertainty estimates, which have skill in distinguishing low-error and high-error situations.

ATMOSPHERIC MEASUREMENT TECHNIQUES (2023)

Article Environmental Sciences

African smoke particles act as cloud condensation nuclei in the wintertime tropical North Atlantic boundary layer over Barbados

Haley M. Royer, Mira L. Poehlker, Ovid Krueger, Edmund Blades, Peter Sealy, Nurun Nahar Lata, Zezhen Cheng, Swarup China, Andrew P. Ault, Patricia K. Quinn, Paquita Zuidema, Christopher Poehlker, Ulrich Poeschl, Meinrat Andreae, Cassandra J. Gaston

Summary: By comparing multiple observational campaigns from January to February 2020, this study reveals the importance of African smoke for atmospheric processes and cloud formation over the Caribbean.

ATMOSPHERIC CHEMISTRY AND PHYSICS (2023)

No Data Available