Closing the Water Vapor Exchange Budget Between the Ice Sheets and Free Atmosphere
As the Arctic warms faster than the rest of the planet, understanding the Greenland ice sheet response to changing climate ? and the associated effect on sea level rise - is important for policy and mitigation strategies. A variety of satellite and surface tools currently exist to help understand snow accumulation and the loss of ice from outlet glaciers or melting, but the magnitude of water vapor exchange between the interior ice sheet and the atmosphere remains essentially unknown. This vapor flux could potentially be a very large factor in calculating the mass gain or loss of the ice sheet. Vapor flux occurs either by addition to the ice surface through vapor deposition and condensation or losses due to sublimation. This project seeks to utilize Unmanned Aerial Vehicles, commonly referred to as drones, for collecting atmospheric water vapor samples to constrain vapor flux on the Greenland Ice Sheet. A remote-controlled sampling pod containing multiple air-capture chambers and environmental sensors will be retrofitted to a commercially available multi-copter drone and flown above the ice surface to collect samples. Upon landing, the atmospheric samples will be analyzed for water isotopes, which are variations of water molecules with different molecular weights that can, for example, provide evidence of vapor flux into or away from the ice sheet. The goal of this project is to use drone-captured data to address major gaps in the understanding of frozen water storage on the Greenland ice sheet, which could reduce uncertainty in estimates of global sea level rise. The data can also be used to improve satellite algorithms used for high-latitude measurements of water isotopes; to improve general circulation models; and improve meteorological understanding of the atmosphere in general. Further, these data may also substantiate the current understanding of long-term temperature records recovered from water isotopes of polar ice cores. Initial testing and atmospheric measurements using the drone-sampling unit will occur in Summer 2018 at an ice core camp in Northeast Greenland. A second deployment in 2019 will allow for improvements to the drone-sampling unit, and a possible deployment of a fixed wing drone aircraft, for measurement of high-resolution data across the 4-month summer field season.
This project will result in the first drone retrofitted with a water vapor sampling pod, which can be directly analyzed in the field following flight. In doing so, the project stands to provide the first detailed and high-resolution airborne measurements of water vapor isotopes in the critical atmospheric boundary layer just above the Greenland Ice Sheet. This region is typically too expensive and dangerous for manned-flight missions, and balloon release experiments have proven logistically burdensome with limited scientific returns. This study brings together researchers from the fields of Aerospace Engineering and Geochemistry. Students and researchers will receive drone pilot training through a Federal Aviation Administration accredited class. Undergraduate and graduate students will receive laboratory training to assist in processing and interpreting the data. A near real-time blog for public viewing and outreach will be available during field operations, which will include field updates, selected data, photography, and film. Public lectures and scientific talks will further disseminate the knowledge learned during this project. As the technology for this project progresses, it could be transferred to other projects, such as detection of fugitive emissions from oil and gas wells or to measure methane release in regions of thawing permafrost.
This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
Through the use of unmanned aerial vehicles (UAVs), this EAGER project seeks to lay the groundwork for major advancements in the understanding of water vapor exchange in the free troposphere, the planetary boundary layer, and the near-surface ice and snow of the Greenland Ice Sheet. The project is a proof-of-concept study to combine concurrent measurements of snow at the ice sheet surface and atmospheric water vapor measurements up to 500 meters in altitude. Researchers will travel to EGRIP in 2019 between the months of May through August to work with their UAV that will be flying in the area of EGRIP. They will be trained in flying the drone as well as interpreting the data in their onsite lab. Travel for team members will be covered under NSF grant #1804154 (Sowers) as this project will share field team members. See Sowers for more information. Travel was cancelled in 2020 and 2021 due to travel restrictions related to COVID-19. Via NSF supplement #2131382 a field team of six will travel under this project (#1833165) via Air National Guard (ANG) to the East Greenland Ice-core Project (EGRIP) camp in 2022. Researchers will travel to EGRIP in 2022 between the months of May through July to work with their fixed-wing UAV that will be operational in the area of EGRIP. They will fly the drone throughout the day making vertical profiles into the atmospheric boundary layer, collecting air samples, and analyzing the isotopes in their onsite lab. Additional samples and data will be collected continuously from a small meteorological tower.
For 2022, Battelle ARO will provide COVID-19 mitigation support (quarantine guidance, lodging, per diem, and testing), field gear, and ANG support for passengers and cargo to Kangerlussuaq and EGRIP. All other logistics will be arranged and paid for by the PI from the research grant.
Research Collaborator(s)
Project Outcomes
This EAGER project has explored the use of Unmanned Aerial Systems (UASs) in the Arctic, laying the groundwork for significant advancements in our understanding of water vapor and water-vapor isotope exchange between the Greenland Ice Sheet and overlying atmosphere. We developed and tested new methods for sampling the atmosphere in places previously inaccessible or difficult to measure. This high-risk-high-reward project made it possible to probe the atmospheric boundary in the half kilometer above the ice, where moisture is added to or subtracted from the ice sheet. In our final field season, we performed over 105 flights, generating samples and vertical profiles of atmospheric conditions (see attached image of figure 3. from Rozmiarek et al., in review). Our work informs the development of the physics of water-isotopes in isotope-enabled models that can help predict Arctic hydrology and future change. We revealed there is a sublimation effect imprinted on water isotopes near the surface of the ice sheet that is not included in certain models. We also found deficiencies in models related to isotope distillation as clouds and vapor move through the climate system. These model shortcomings need to be improved so that we can better predict hydrologic cycle changes in the future. Our results also shed light on how climate information is passed back and forth from the atmosphere to the ice, and ultimately this information reveals climate histories in deeper ice recovered in ice core drilling programs. We have long known that examination of preserved past precipitation events (snow) on ice sheets can document climate history. For example, water isotopes are a proxy for historical temperature. But our data now help to show that the relationship between the atmosphere and ice is complex and is very much a two-way exchange, with each influencing the physics of the other. Further unraveling this relationship may someday allow for a deeper understanding of the nuances of climate history as recorded in ice cores. Our results have also provided important comparisons with atmospheric models to help validate the physics surrounding our understanding of water vapor transport in general, which is a cornerstone for understanding today’s climate and interpreting the climate dynamics and Earth’s climate history.
The overall results of this project are numerous and include A) Technological advances in remote sampling from UAS platforms, B) Training of students and technicians, who will be tomorrow’s scientists and UAS pilots, C) Presentations at both public forums and professional meetings and D) Documentation of our findings in peer-reviewed journals. E) We have submitted a proposal to expand this study in another part of Greenland. F) This project inspired UAS sampling applications for similar measurements that we are making in Alaska to measure methane from permafrost.
To achieve our results, we had to overcome a variety of challenges, ranging from technical hurdles, conducting field operations in extreme cold environments, arranging permission to legally fly drones at high altitudes (up to 1500 meters), mitigating magnetic compass disturbances at high latitudes (>75°N), and, of course, restrictions stemming from the pandemic. We believe this project and its outcomes embrace the true spirit of the EAGER program, to sponsor ideas that are high-risk-high-reward projects on the bleeding edge of development, to achieve novel results.