Measurements at the Mauna Loa Observatory stopped after the 2022 eruption of the Mauna Loa volcano, when lava flow crossed the access road and took out power lines to the facility. The observatory remains inaccessible by vehicle and without power from the local utility company.
Observatory staff has established limited solar power in four observatory buildings and restored approximately 33 percent of the measurements onsite, including the Global Monitoring Laboratory and Scripps critical CO2 records and other atmospheric measurements.
Media can contact: Theo Stein (303) 819-7409 (theo.stein@noaa.gov) or Karin Vergoth 303-632-6413 (karin.vergoth@noaa.gov)
Network For the
Detection of Atmospheric Composition Change (NDACC)
Naval Research
Laboratory
NASA (National Aeronautics and Space Administration),
U.S. Department of DefenseThe goal of the Water Vapor Millimeter-wave Spectrometer (WMVS) project is to measure water vapor in the middle atmosphere (between about 40 and 80 km), in parts per million. Since water vapor is the primary source of the hydroxide (OH) radical and other hydrogen compounds, it is important in controlling ozone chemistry. Because the chemical time scales for water vapor are long relative to time scales for transport in the middle atmosphere, it is also an excellent tracer of atmospheric motion. Water vapor profiles are obtained by measuring the emission of the 22 GHz transition of water vapor. The data has been obtained from nearly continual observations at the Network for the Detection of Atmospheric Composition Change (NDACC) sites in Table Mountain, California (Jan. 1992 - Nov 1997, Nov. 2003-present), in Lauder, New Zealand (since November 1992), and in Mauna Loa, Hawaii (since February 1996).
The WVMS instrument is a microwave radiometer which measures water vapor emission at 22 Ghz with filters ranging from 200 kHz to 14 MHz, and a total bandwidth of 420 MHz. The measurements allow for the retrieval of water vapor mixing ratios with a resolution of 10-15 km at altitudes of 40-80 km. The system is computer controlled, with data brought back to NRL via a modem link. The instrument is calibrated weekly using an ambient and a liquid nitrogen target, and run continuously at MLO.
Water vapor plays a role both in the radiative and chemical balance of the middle atmosphere. Long-term changes in the amount of water vapor in the stratosphere can affect stratospheric temperatures, while its role as a reservoir of odd hydrogen makes it directly important to ozone chemistry. In the mesosphere water vapor provides a good tracer of atmospheric transport. These measurements are important primarily for trend detection and as an independent calibration of satellite trend detection.
Large (2% per year) trends were observed in the early 1990s, but there has been no significant change since about 1996. Some of these trends are caused by changes in methane (CH4) and by changes in atmospheric transport, but about half of the 2% per year trend in the early 1990s is still not fully explained. In 2001 a decrease in lower stratospheric water vapor was detected in lower altitude datasets, but this decrease has to date not been clearly detected at the altitudes measured by WVMS.
Long-term changes in water vapor will affect ozone and therefore stratospheric temperatures. Also, the amount of water vapor in the middle atmosphere is very sensitive to temperature at the tropical tropopause.
Mauna Loa is an ideal site for these measurements both because its low latitude reduces the seasonal cycle (and thus makes trend detection easier) and because the high altitude reduces the amount of tropospheric water which we need to look through.
Dr. Gerald Nedoluha
202-767-4246
Mike Gomez
202-767-3533
Dr. John E. Barnes
808-933-6965 (x222)
1996
