ARL Weekly News – November 18, 2022
NADP Fall Meeting and Scientific Symposium
LaToya Myles, Rick Saylor and Nebila Lichiheb attended the NADP conference in Knoxville, TN from November 14-18, 2022: https://nadp.slh.wisc.edu/nadp2022/.
Bruce Hicks, former ARL director and current collaborator, also attended the NADP conference and made an oral presentation entitled “Dry Deposition in NADP: On Rekindling the Flame”.
The scientific symposium was a great opportunity to meet with our EPA collaborators and discuss future collaborations.
Also at NADP on November 17, Dr. Patrick Campbell gave a virtual presentation on “Pronounced increases in nitrogen emissions and deposition due to the historic 2020 wildfires in the western U.S,” on the following research highlights:
- The August-October 2020 “gigafires” contributed up to 83% of the total nitrogen emissions in the western U.S.
- These extreme biomass burning emissions led to a 78% relative increase in annual average nitrogen deposition to major vegetation types in California.
- The relative increase in nitrogen deposition is even larger to mixed forests in California at 173%, with annual average deposition rates about 6-12 times larger than low-end critical loads (1.5 – 3 kg ha-1 yr-1).
ARL’s Mobile Measurement Survey of DC/Baltimore
Phil Stratton and Xinrong Ren were interviewed by Aman Azhar, a reporter from Inside Climate News, while they were conducting a mobile measurement survey in Washington, DC on November 21. During the interview, they talked about NOAA ARL’s Greenhouse Gas (GHG) program and the science and policy relevance of the mobile and aircraft measurements of GHGs. They also talked about how the mobile measurements of air pollutants can help address environmental justice issues in some local communities in Washington, DC and Baltimore.
ARL’s Plume Lab and Air Research Car
On Wednesday November 16, three students from Montgomery Blair High School toured ARL and the NESDIS Operations Center. They are working on an article about climate research and on how NOAA monitors the atmosphere and oceans for Silver Chips, Montgomery Blair High School’s student newspaper. They interviewed Howard Diamond on his role in NOAA, the agency’s climate observation methods and the government’s role in monitoring the Earth’s atmosphere. The students toured the plume lab and the ARL lab space and instrumentation. Xinrong Ren walked them through the goals and instruments on NOAA’s Air Research Car, or ARC.
University of Alabama Climate Outreach
John Kochendorfer gave a talk to a dozen UofA students for a class on climate change, and gave an overview of climate science and ARL’s climate measurements.
NSF Greenhouse Gas Workshop
Chris Loughner virtually participated in the NSF Greenhouse Gas Workshop November 16-17 to help identify research needs in order to improve greenhouse gas emissions estimates. Dr. Loughner led a breakout group that identified processes that need to be better represented in models to minimize location and quantification uncertainties of greenhouse gas emissions estimates. Over the next month, workshop participants will develop and deliver a workshop final report to NSF.
In situ Soil Moisture Sensors in Undisturbed Soils
Caldwell, T. G., Cosh, M. H., Evett, S. R., Edwards, N., Hofman, H., Illston, B. G., Meyers, T., Skumanich, M., Sutcliffe, K. In situ Soil Moisture Sensors in Undisturbed Soils. J. Vis. Exp. (189), e64498, doi:10.3791/64498 (2022).
Abstract: Soil moisture directly affects operational hydrology, food security, ecosystem services, and the climate system. However, the adoption of soil moisture data has been slow due to inconsistent data collection, poor standardization, and typically short record duration. Soil moisture, or quantitatively volumetric soil water content (SWC), is measured using buried, in situ sensors that infer SWC from an electromagnetic response. This signal can vary considerably with local site conditions such as clay content and mineralogy, soil salinity or bulk electrical conductivity, and soil temperature; each of these can have varying impacts depending on the sensor technology.
Furthermore, poor soil contact and sensor degradation can affect the quality of these readings over time. Unlike more traditional environmental sensors, there are no accepted standards, maintenance practices, or quality controls for SWC data. As such, SWC is a challenging measurement for many environmental monitoring networks to implement. Here, we attempt to establish a community-based standard of practice for in situ SWC sensors so that future research and applications have consistent guidance on site selection, sensor installation, data interpretation, and long-term maintenance of monitoring stations.
The videography focuses on a multi-agency consensus of best-practices and recommendations for the installation of in situ SWC sensors. This paper presents an overview of this protocol along with the various steps essential for high-quality and long-term SWC data collection. This protocol will be of use to scientists and engineers hoping to deploy a single station or an entire network.
Vertical profiles of cloud condensation nuclei number concentration and its empirical estimate from aerosol optical properties over the North China Plain
Zhang, R., Wang, Y., Li, Z., Wang, Z., Dickerson, R. R., Ren, X., He, H., Wang, F., Gao, Y., Chen, X., Xu, J., Cheng, Y., and Su, H.: Vertical profiles of cloud condensation nuclei number concentration and its empirical estimate from aerosol optical properties over the North China Plain, Atmos. Chem. Phys., 22, 14879–14891, https://doi.org/10.5194/acp-22-14879-2022, 2022.
Abstract: To better understand the characteristics of aerosol activation ability and optical properties, a comprehensive airborne campaign was conducted over the North China Plain (NCP) from 8 May to 11 June 2016. Vertical profiles of cloud condensation nuclei (CCN) number concentration (NCCN) and aerosol optical properties were measured simultaneously. Seventy-two-hour air mass back trajectories show that during the campaign, the measurement region was mainly influenced by air masses from the northwest and southeast. Air mass sources, temperature structure, anthropogenic emissions, and terrain distribution are factors influencing NCCN profiles. Cloud condensation nuclei spectra suggest that the ability of aerosol to activate into CCN is stronger in southeasterly air masses than in northwesterly air masses and stronger in the free atmosphere than near the surface. Vertical distributions of the aerosol scattering Ångström exponent (SAE) indicate that aerosols near the surface mainly originate from primary emissions consisting of more fine particles. The long-distance transport decreases SAE and makes it vary more in the free troposphere than near the surface. To parameterize NCCN, the equation is used to fit the relationship between NCCN and the aerosol scattering coefficient (σ) at 450 nm. The fitting parameters β and γ have linear relationships with the SAE. Empirical estimates of NCCN at 0.7 % water vapor supersaturation (SS) from aerosol optical properties are thus retrieved for the two air masses: for northwesterly air masses and for southeasterly air masses. The estimated NCCN at 0.7 % SS agrees with that measured, although the performance differs between low and high concentrations in the two air masses. The results highlight the important impact of aerosol sources on the empirical estimate of NCCN from aerosol optical properties.