Microwave Limb Sounder (MLS) experiments measure naturally-occurring microwave thermal emission from the limb (edge) of Earth's atmosphere to remotely sense vertical profiles of atmospheric gases, temperature, pressure, and cloud ice. The overall objective of these experiments is to provide information that will help improve our understanding of Earth's atmosphere and global change.

Aura MLS Data

MLS "190 GHz" Observations Status

This is an update on the status of the MLS “190 GHz” observations, mainly H2O and N2O (also HCN and upper stratospheric HNO3). The electronics making these measurements has been aging since around 2010, leading to a drift in the MLS H2O and N2O products in the MLS v4 record. This drift was ameliorated (more so for H2O than N2O) in the v5 dataset. Unfortunately, the aging has now reached a point such that we believe there are only about 4-6 months' worth of reliable observations left from the MLS 190 GHz receiver. The good news is that we are very confident that powering the receiver down will conserve its remaining life. Note that, due to limitations in fuel/orbit/power, both MLS and the Aura mission as a whole are expected to cease operations by the end of May 2026. Accordingly, we plan to “duty cycle” the MLS 190 GHz measurements to enable them to extend through to the end of Aura's lifetime (albeit with interruptions). We have considered various strategies for this duty cycling. Our current plan is to activate the 190 GHz measurements for about six days at a time on a roughly monthly cadence (precise details to be determined based on a variety of factors). We may decrease (or increase) the number of days of activation depending on how the aging progresses. We anticipate powering down the 190 GHz subsystem early this week (week of April 29th, 2024) with our first reactivation period planned for mid-to-late May. A reminder that the only Aura MLS products affected by this issue are H2O, N2O, HCN, and upper stratospheric HNO3. All other products (e.g., O3, HCl, ClO, CO) are unaffected.

UPDATED - Aura MLS v4 Production Ending in May 2024

The science team for the Microwave Limb Sounder (MLS) on NASA's Aura satellite is finalizing new “Version 6” (V6) data processing algorithms and software. We anticipate releasing V6 MLS data in summer 2024, once its quality has been assessed and documented. Reprocessing of the entire (19-year-to-date) MLS record with the V6 software will take approximately two years, completing in mid-2026. During that time, we will continue to process incoming MLS data with the current V5 algorithms and software, thus ensuring uninterrupted availability of a uniform MLS dataset encompassing the full mission lifetime. However, to maximize the computing resources available for V6 reprocessing, we will cease processing the incoming data with the older V4 algorithms and software. The last V4 data generated will be for May 31, 2024.

Recent Publications

  1. Pan, H., G. Ren, M. Wang, J. Wang, and K. Kumar, "Investigation on the spatiotemporal and vertical structure of ice cloud and aerosol parameters from multi-source satellite datasets 2007–2021 over the Tarim Basin, China," J. Atmos. Solar-Terr. Phys. 256, 106185, doi:10.1016/j.jastp.2024.106185, 2024.
  2. Salminen, A., T. Asikainen, and K. Mursula, "Satellite Observations of the Influence of Energetic Electron Precipitation on the Mesosphere and Stratosphere in the Northern Hemisphere," Journal of Geophysical Research: Atmospheres 129, 7, doi:10.1029/2023jd039581, 2024.
  3. Orfanoz-Cheuquelaf, A., C. Arosio, A. Rozanov, M. Weber, A. , J. Burrows, A. Thompson, R. Stauffer, and D. Kollonige, "Tropospheric ozone column dataset from OMPS-LP/OMPS-NM limb–nadir matching," Atmospheric Measurement Techniques 17, 6, 1791-1809, doi:10.5194/amt-17-1791-2024, 2024.
  4. Zhang, J., D. Kinnison, Y. Zhu, X. Wang, S. Tilmes, K. , and W. Randel, "Chemistry Contribution to Stratospheric Ozone Depletion After the Unprecedented Water‐Rich Hunga Tonga Eruption," Geophys. Res. Lett. 51, 7, doi:10.1029/2023gl105762, 2024.
  5. Ploeger, F., T. Birner, E. Charlesworth, P. Konopka, and R. , "Moist bias in the Pacific upper troposphere and lower stratosphere UTLS in climate models affects regional circulation patterns," Atmos. Chem. Phys. 24, 3, 2033-2043, doi:10.5194/acp-24-2033-2024, 2024.