Remote sensing of atmospheric HDO/H2O in southern California from CLARS-FTS. (September 2022)

• Record Type: Journal Article
• Authors: Zeng, Zhao-Cheng; Addington, Olivia; Pongetti, Thomas; Herman, Robert L.; Sung, Keeyoon; Newman, Sally; Schneider, Andreas; Borsdorff, Tobias; Yung, Yuk L.; Sander, Stanley P.
• Is Part Of: Journal of quantitative spectroscopy & radiative transfer. Volume 288(2022)
• Publication Date: 2022-09
• Subjects: Remote sensing -- Atmospheric isotopologues -- HDO -- Planetary boundary layer -- Los Angeles -- CLARS; Spectrum analysis -- Periodicals; Radiation -- Periodicals; Analyse spectrale -- Périodiques; Rayonnement -- Périodiques; Radiation; Spectrum analysis; Periodicals; 543.0858
• DOI: 10.1016/j.jqsrt.2022.108254
• Languages: English
• ISSNs: 0022-4073

Abstract

Highlights: Retrievals of HDO, H2 O, and δD were made over southern california by CLARS-FTS from 2011 to 2019. The δD values show a significant seasonal cycle that is highly correlated with the change of atmospheric absolute humidity. δD retrievals by CLARS-FTS, TCCON, and TROPOMI are in good agreement. Abstract: Atmospheric isotopologues of water vapor (e.g., HDO) are important tracers for understanding Earth's hydrological cycles. Most remote sensing and in-situ measurements of these isotopologues, however, are either column averaged values or sparse in space and time. Measurements targeting the planetary boundary layer (PBL), the part of the atmosphere that has high sensitivity to surface sources of water vapor isotopologues, are much rarer. In this study, we retrieved HDO and H2 O columns from observations by the California Laboratory for Atmospheric Remote Sensing Fourier Transform Spectrometer (CLARS-FTS), a mountaintop observatory on Mt. Wilson (1.67 km a.s.l.) overlooking the Los Angeles (LA) basin in southern California. CLARS-FTS observations are highly sensitive to the lower atmosphere due to the long light path along the PBL. Retrievals were conducted using spectral windows between 6000 and 7000 cm −1 from CLARS-FTS observations (2011–2019). The isotopological abundance δD, which represents the relative difference of the HDO/H2 O ratio to a standard abundance ratio, is also calculated. The averaged δD retrievals are (−156.1 ± 60.0)‰ with an uncertainty of (6.1 ± 10.2)‰ for LA Basin Survey mode and (−344.7 ± 95.0)‰ with an uncertainty of (42.4 ± 31.6)‰ for Spectralon Viewing Observation mode. In LA, the δD shows a seasonal cycle that is primarily driven by the change of atmospheric humidity. A comparison analysis shows that the δD measurements by CLARS-FTS, a collocated Total Carbon Column Observing Network (TCCON), and the TROPOspheric Monitoring Instrument (TROPOMI) are in good agreement. The difference between CLARS and TCCON δD retrievals can primarily be attributed to the difference in their observation geometries. We envision that the HDO and δD measurements from CLARS-FTS provide high spatial and temporal resolution datasets for further study of hydrological processes, such as the partitioning of the water flux into soil evaporation and transpiration, standing water evaporation, or transport and mixing from the oceans, in the LA megacity.