NOAA's National Centers for Environmental Information
Tropopsphere
Mid-troposphere
| March | Anomaly |
Rank
(46 years)
|
Record Years | Decadal Trend | |||||
|---|---|---|---|---|---|---|---|---|---|
| °C | °F | Year | °C | °F | °C | °F | |||
| STAR | +0.89 | +1.60 | Coolest | 46th | 1993 | -0.35 | -0.63 | +0.08 | +0.15 |
| Warmest | 1st | 2024 | +0.68 | +1.22 | |||||
| January– |
Anomaly |
Rank
(46 years*)
|
Record Years | Decadal Trend | |||||
|---|---|---|---|---|---|---|---|---|---|
| °C | °F | Year | °C | °F | °C | °F | |||
| STAR | +0.88 | +1.58 | Coolest | 46th | 1984, 1993 | -0.26 | -0.47 | +0.09 | +0.17 |
| Warmest | 1st | 2024 | +0.64 | +1.15 | |||||
| RATPAC* | +1.34 | +2.41 | Coolest | 67th | 1965 | -0.89 | -1.60 | +0.19 | +0.34 |
| Warmest | 1st | 2024 | +1.15 | +2.07 | |||||
*RATPAC rank is based on 67 years of data
Stratosphere
Lower Stratosphere
| March | Anomaly |
Rank
(46 years)
|
Record Years | Decadal Trend | |||||
|---|---|---|---|---|---|---|---|---|---|
| °C | °F | Year | °C | °F | °C | °F | |||
| STAR | -0.52 | -0.94 | Coolest | 4th | 1999 | -0.62 | -1.12 | -0.22 | -0.39 |
| Warmest | 43rd | 1983, 1992 | +1.18 | +2.12 | |||||
| January– |
Anomaly |
Rank
(46 years)
|
Record Years | Decadal Trend | |||||
|---|---|---|---|---|---|---|---|---|---|
| °C | °F | Year | °C | °F | °C | °F | |||
| STAR | -0.45 | -0.81 | Coolest | 6th | 2012 | -0.56 | -1.01 | -0.23 | -0.41 |
| Warmest | 40th | 1983 | +1.30 | +2.34 | |||||
| Ties: 2021 | |||||||||
Background
Temperatures above the Earth's surface are measured within the lower troposphere, middle troposphere, and stratosphere using in-situ balloon-borne instruments (radiosondes) and polar-orbiting satellites (NOAA's TIROS-N). The radiosonde and satellite records have been adjusted to remove time-dependent biases (artificialities caused by changes in radiosonde instruments and measurement practices as well as changes in satellite instruments and orbital features through time). Global averages from radiosonde data are available from 1958 to present, while satellite measurements date back to 1979.
The mid-troposphere temperatures are centered in the in the atmospheric layer approximately 3–10 km [2–6 miles] above the Earth's surface, which also includes a portion of the lower stratosphere. (The Microwave Sounding Unit [MSU] channel used to measure mid-tropospheric temperatures receives about 25 percent of its signal above 10 km [6 miles].) Because the stratosphere has cooled due to increasing greenhouse gases in the troposphere and losses of ozone in the stratosphere, the stratospheric contribution to the tropospheric average, as measured from satellites, creates an artificial component of cooling to the mid-troposphere temperatures. The University of Washington (UW) versions of the UAH and RSS analyses attempt to remove the stratospheric influence from the mid-troposphere measurements, and as a result the UW versions tend to have a larger warming trend than either the UAH or RSS versions. For additional information, please see NCEI's Microwave Sounding Unit page.
The radiosonde data used in this global analysis were developed using the Lanzante, Klein, Seidel (2003) ("LKS") bias-adjusted dataset and the First Difference Method (Free et al. 2004) (RATPAC). Additional details are available. Satellite data have been adjusted by the Global Hydrology and Climate Center at the University of Alabama in Huntsville (UAH). An independent analysis is also performed by Remote Sensing Systems (RSS) and a third analysis has been performed by Dr. Qiang Fu of the University of Washington (UW) (Fu et al. 2004)** to remove the influence of the stratosphere on the mid-troposphere value. Global averages from radiosonde data are available from 1958 to present, while satellite measurements began in 1979.
References
- Christy, John R., R.W. Spencer, and W.D. Braswell, 2000: MSU tropospheric Temperatures: Dataset Construction and Radiosonde Comparisons. J. of Atmos. and Oceanic Technology, 17, 1153-1170.
- Free, M., D.J. Seidel, J.K. Angell, J. Lanzante, I. Durre and T.C. Peterson (2005) Radiosonde Atmospheric Temperature Products for Assessing Climate (RATPAC): A new dataset of large-area anomaly time series, J. Geophys. Res., 10.1029/2005JD006169.
- Free, M., J.K. Angell, I. Durre, J. Lanzante, T.C. Peterson and D.J. Seidel(2004), Using first differences to reduce inhomogeneity in radiosonde temperature datasets, J. Climate, 21, 4171-4179.
- Fu, Q., C.M. Johanson, S.G. Warren, and D.J. Seidel, 2004: Contribution of stratospheric cooling to satellite-inferred tropospheric temperature trends. Nature, 429, 55-58.
- Lanzante, J.R., S.A. Klein, and D.J. Seidel (2003a), Temporal homogenization of monthly radiosonde temperature data. Part I: Methodology, J. Climate, 16, 224-240.
- Lanzante, J.R., S.A. Klein, and D.J. Seidel (2003b), Temporal homogenization of monthly radiosonde temperature data. Part II: trends, sensitivities, and MSU comparison, J. Climate, 16, 241 262.
- Mears, Carl A., F.J. Wentz, 2009, Construction of the RSS V3.2 lower tropospheric dataset from the MSU and AMSU microwave sounders. Journal of Atmospheric and Oceanic Technology, 26, 1493-1509.
- Mears, Carl A., F.J. Wentz, 2009, Construction of the Remote Sensing Systems V3.2 atmopsheric temperature records from the MSU and AMSU microwave sounders. Journal of Atmospheric and Oceanic Technology, 26, 1040-1056.
- Mears, Carl A., M.C. Schabel, F.J. Wentz, 2003: A Reanalysis of the MSU Channel 2 tropospheric Temperature Record. J. Clim, 16, 3650-3664.
- Zou, C.-Z., M. Goldberg, Z. Cheng, N. Grody, J. Sullivan, C. Cao, and D. Tarpley (2006) Recalibration of microwave sounding unit for climate studies using simultaneous nadir overpasses, J. Geophys. Res., 111, D19114, DOI:10.1029/2005JD006798.
- Zou, Cheng-Zhi and Wenhui Wang (2011), Inter-satellite calibration of AMSU-A observations for weather and climate applications, J. Geophys. Res., 116, D23113, DOI:10.1029/2011JD016205.