pubmed.ncbi.nlm.nih.gov

The need for accurate long-term measurements of water vapor in the upper troposphere and lower stratosphere with global coverage - PubMed

The need for accurate long-term measurements of water vapor in the upper troposphere and lower stratosphere with global coverage

Rolf Müller et al. Earths Future. 2016 Feb.

Abstract

Water vapor is the most important greenhouse gas in the atmosphere although changes in carbon dioxide constitute the "control knob" for surface temperatures. While the latter fact is well recognized, resulting in extensive space-borne and ground-based measurement programs for carbon dioxide as detailed in the studies by Keeling et al. (1996), Kuze et al. (2009), and Liu et al. (2014), the need for an accurate characterization of the long-term changes in upper tropospheric and lower stratospheric (UTLS) water vapor has not yet resulted in sufficiently extensive long-term international measurement programs (although first steps have been taken). Here, we argue for the implementation of a long-term balloon-borne measurement program for UTLS water vapor covering the entire globe that will likely have to be sustained for hundreds of years.

PubMed Disclaimer

Figures

Figure 1
Figure 1

Potential temperature-based (10 K bins) frequency distribution of water vapor mixing ratios from 23 aircraft campaigns measured with the Fast In-situ Stratospheric Hygrometer (FISH) hygrometer [Meyer et al., 2015] from 1997 to 2014 divided into three latitude regimes: tropical (30°S to 30°N), sub-tropical (60°S to 30°S and 30°N to 60°N), and polar regions (90°S to 60°S and 60°N to 90°N). The number of data points (measurements every second) is given at the top right of the respective panel.

Figure 2
Figure 2

Stratospheric water vapor between 1981 and 2014 from Boulder sonde data (Hurst et al., 2011; Kunz et al., 2013). Top panel (a) shows data for 75–85 hPa (≈18 km); the panels below show subsets of the data selected according to the altitude level of the tropopause at the individual sounding. Second panel (b) shows data for the tropical domain (tropopause greater than 14 km); third panel (c) for a transitional domain (tropopause between 14 and 12 km); and bottom panel (d) data for the extratropical domain (tropopause below 12 km). The black line in the top panel shows water vapor monthly means; 2-year running means in all panels are shown in orange. Also shown are corresponding HALOE data for 1991–2005 (zonal average of the latitude band 35°N to 45°N); the white line shows the 2-year running mean; the range of two standard deviations around the mean is shown as gray shading [Kunz et al., 2013]. Note that around the year 2000, no data are available for tropopause greater than 14 km (panel b). (Figure adapted from Kunz et al. [2013]; see reference for further information on the analysis).

Similar articles

Cited by

References

    1. Anderson J, Wilmouth D, Smith J, Sayres D. UV dosage levels in summer: Increased risk of ozone loss from convectively injected water vapor. Science. 2012;337(6096):835–839. doi: 10.1126/science.1222978. - DOI - PubMed
    1. Brabec M, Wienhold FG, Luo BP, Vömel H, Immler F, Steiner P, Hausammann E, Weers U, Peter T. Particle backscatter and relative humidity measured across cirrus clouds and comparison with microphysical cirrus modelling. Atmos Chem Phys. 2012;12(19):9135–9148. doi: 10.5194/acp-12-9135-2012. - DOI
    1. Brogniez H, Clain G, Roca R. Validation of upper-tropospheric humidity from SAPHIR on board Megha-Tropiques using tropical soundings. J Appl Meteorol Climatol. 2015;54:896–908. doi: 10.1175/JAMC-D-14-0096.1. - DOI
    1. Chung ES, Soden B, Sohn BJ, Shi L. Upper-tropospheric moistening in response to anthropogenic warming. Proc Natl Acad Sci U S A. 2014;111(32):11,636–11,641. - PMC - PubMed
    1. Davis SM, Rosenlof KH, Hurst DF. Stratospheric water vapor. Bull Am Meteorol Soc. 2015;96(7):S46–S48.

LinkOut - more resources