Homogenized radiosonde temperature data for climate reanalyses

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Homogenized radiosonde temperature data for climate reanalyses L Haimberger University of Vienna, Austria Thanks to H Hersbach, P Dahlgren S Brönnimann, S Jourdain, M. A. Valente, A. Sterin, F. Ladstätter A. Steiner

Motivation for an update Radiosonde data need homogenization RAOBCORE adjustments (Haimberger 2012) only back to 1958 up to 2011 More early upper air data available since then Many paper archives have been digitized 5 year longer records New reference data for break detection/adj. JRA55 (1958-), ERA-preSAT (1939-1966) CERA20C (1900-2010) Improved homogenization methods Annual cycle of bias

Radiosonde temperature monthly records South of 20N North of 20N 2011 2017 2011 2017 Many of the pre-igy data have been digitized only recently (ERA-CLIM(2)) Are now in ODB format - ready for assimilation with Copernicus ERA5 Homogeneity adjustments??

5 Highlights Pervasive biases in pre-satellite era Data may nevertheless be of good quality How do they influence the reference? Near-surface inhomogeneities Influence of GPS-RO data Adjustment of short records Annual cycle of bias

Trends 1949-1969, 300 hpa 230 K/10a

Trends 1954-1974, 300 hpa 368 K/10a

RAOBCORE/RICH Homogenization Break Detection analyzes differences between radiosonde temperature time series and existing reanalysis time series as well as HadCRUT(EM)4 temperatures Automatic break detection with SNHT Break Adjustments using Reanalyses time series as reference (RAOBCORE) Neighbouring RS time series as reference (RICH) Adjustment of whole series if most recent part is biased also short records adjusted

Reference series There is no perfect reference series eijra_fgdep: ERA-preSAT 1939-66, JRA55 1967-78, ERA-Interim 1979- Transition adjustments: 4yr parallel (1963-66, 1979-83, adjustments for each month) eice20c_andep: Ensemble mean CERA20C analyses 1939-78, ERA-Interim 1979- jrace20c_andep: CERA20C analyses 1939-1978, JRA55 1979- Radiosonde composites (RICH)

RAOBCORE/RICH Reference eijra: EI+JRA55+preSAT Reference jrace20c: JRA55+CERA20C SONDES 260630RZ049 194501009941 SONDES 260630A22 1959030099 1 SONDES 260630RKZ-1 1962050099 1 SONDES 260630RKZ-2 1972110099 1 SONDES 260630MARS 1985020099 SONDES 260630MRZ 1991010099 1 ERA presat JRA55 ERA-Interim CERA20C JRA55

Trend ERA-preSAT+JRA55 1954-1974

Trends CERA20C 1954-1974

Adjusted trends 1954-1974

Unadj.Trends 1954-1974, 300 hpa

Effect on zonal mean trends 1954-1974 before adjustment 1954-1974 after adjustment

Adjustment FSU using different reference series FSU 1948-1985 Difference series to unadjusted radiosondes 1.5K bias! Adjustment suggested both by CERA20C, RICH JRA55/ERApreSAT as reference Breaks detected but not adjusted! RICH still works here!

850 hpa temperatures in Tropics Differences to unadjusted radiosonde series? RS 850 hpa temperature 0.5K too cool in Tropics? Not only vs. Reanalyses but also vs. HadCRUT4

Some very cool temperatures over Africa? Difference radiosonde-reanalysis 1959-1960, 850 hpa Unadj. Adj.

Comparisons for Satellite Era: MSU TLS K ERAI bg reference K JRA bg reference Better fit!

Pre-COSMIC to COSMIC, 100 hpa cosmic GPS-RO from CDAAC (Boulder) and Wegener Center (Graz) ERAI cooler than CHAMP RO data until 2007, ERA5 has the same problem JRA55 slightly warmer than RO during CHAMP period Excellent agreement after 2007

20S-20N T-Trends 1958-2010 Good agreement for 1958-2010 Large uncertainty 1969-1989 in stratosphere.

Annual cycle of radiation error At high latitudes, regions around 100W, 80E Estimate radiation error as function of solar elevation Different radiosonde types have different annual cycles of bias Mostly in phase with solar elevation.

Outlook More reliable homogeneity adjustments, 1939- Some large biases could be addressed Consistency with GPS-RO Different references tried CERA20C+JRA55 best compromise Other choices help assessing uncertainties involved Deliverable, to be used in ERA5 http://srvx1.img.univie.ac.at/raobvis/ Humidity M. Blaschek s talk Revisit wind many new PILOTs in early period

Spatial trend consistency

Overall adjustments 1959-1960 CTRL JRA+CERA20C ERAI+JRA+preSAT ERAI+JRA55+preSAT - RICH JRA+CERA20C - RICH

Adjusted Trends 1949-69, 300 hpa

Results from radiosonde intercomparisons Nash and Schmidlin, 1987 Greenbelt, 27 Sept 2005 27

Temperature Differences

Temperature Difference ce20c

Temperature Differences ERA-preSAT