Data trends at meteoLCD: 1998 to 2013
Trends computed from yearly averages at meteoLCD,
Diekirch, Luxembourg.
Graphs may be freely copied and used, under the condition to cite:
MASSEN, Francis: Data trends at meteoLCD, 1998 to 2013. http://meteo.lcd.lu
Older trends are here!
Most important conclusions for the last decade (2004 to 2013) linear trends:
1. Solar dimming is -26 kWh*m-2*decade-1
[- 2.4 %]
2. Local temperatures are declining by -0.15 °C*decade-1 [
- 1.5 %]
3. There is no trend in daily min. temperatures, DTR and daily max. show small
decrease
4. The winters are cooling by -0.71 °C*decade-1
[- 24.7%]
5. Ground O3 increases by 2.1 ug*m-3*decade-1
(suspicious!),
thickness of ozone layer increases by 0.6 DU*decade-1
[+ 0.2%]
6. Local CO2 mixing ratio increases by 3.2 ppmV*decade-1
(suspicious!), by +0.98 ppmV*y-1 from 2002 to 2012 and +0.83 ppmV*y-1
from 2002 to 2013
7. The biologically effective UVB dose declines by 3 eff. Wh*m-2*decade-1
[- 2.3%]
8. The UVA dose declines by 0.3 kWh*m-2*y-1[-
4.0%]
9. Precipitation (rainfall) increases by 77 mm*decade-1
[+ 1.3%]
10. Energy content of moist air (enthalpy) declines by -0.6 KJ*Kg-1*decade-1
[-2.1 %]
11. NO2 concentrations increase by 6 ug*m-3*decade-1
(suspicious) [+ 31%]
12. NO concentrations decrease by -3 ug*m-3*decade-1
[-30 %]
Ground
Ozone [ug/m3] ("bad ozone") From 1998 to 2013: negative trend: -0.7 ug/m3 per year 1998-2013 mean
+/- stdev: Attention: there are about 15% missing data in 2013 due to frequent sensor failures, so the 2013 data point and the 2004-2013 trend line are suspicious!
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Total
Ozone Column [DU] ("good ozone") Mean +/_std: 320.9 +/- 45.8 DU positive trend: +1.6 DU per year, -0.1 since 2002 (Uccle gives +0.95 for the 1998-2010 period) (see also [16]) Calibration multiplier to apply if Uccle Brewer #16 is the reference: 1998 to 2007: * 0.95 2008 to 2010: * 1.00 2011 : * 1.06 2012 : * 1.04 2013 : * 1.06 (provisional) 2013 common days measurements results: Diekirch = 321.6 DU Uccle DS = 342.0 DU Uccle data are from WOUDC (stat.53, Brewer#16, provisional as Dec. data not yet available) 1998 to 2012 mean
+/- stdev: |
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CO2
mixing ratio in ppmV The 1998-2001 data are too unreliable to be retained
for the trend analysis. 2007 to 2013 mean
+/- stdev:: 410.9 +/- 4.2 ppmV
The right picture shows the asymptotic CO2 values
(CO2wind)
derived from the model published in [21] . See also [25]
The 2013 CO2 data clearly show the summer-time lows, mostly due to the increased photo-synthesis. The amplitude 2A of the best-fit sinusoidal model is about 12 ppmV. The paper [35] gives an annual swing of ~12 ppmV whereas the Hohenpeissenberg (lat. 47.8°) and Ochsenkopf (lat. 50°) measurements suggest about 20 ppmV. A paper discussed at [36] gives an 2A amplitude of about 12 ppmV at ~5km altitude and 50° latitude North. It seems that the annual swing is increasing since 1960 mostly due to enhanced biosphere activity. |
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Air
temperature [°C]
Trend from 1998 to 2013: +0.0045 °C per year, practically flat! 1998 to 2013 mean
+/- stdev::
2002 to 2013: The sensor has
not been moved since 2002! |
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Diurnal
Temperature Range (DTR) [°C]
DTR = daily max - daily min temperature 1998 to 2012 mean
+/- stdev:: 8.48 +/- 0.55 °C
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Winter
temperatures [°C] Contrary to what is often suggested in the media, winters are cooling since 2002. The cooling rates per decade are: Diekirch: -0.46 °C/decade The plot shows the mean temperatures of
December (from previous year), January and February. It also shows in
brown (right Y-axis) the NAO index for the months Dec to Mar [32] |
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Total
Yearly Rainfall [mm]
1998 to 2013 mean +/- stdev::mean : |
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Solar
energy on a horizontal plane mean
+/ std:: 1109.8 +/-46.5 kWhm-2
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Sunshine
duration (derived from pyranometer data by Olivieri's method)
Totals for 2013: The decline from 2012 to 2013 is -10.8%, to be compared to the data from the Fraunhofer Institut which give a decline of -10.6 % of the German PV "Volllasttunden" [37]
See paper
[23] by F. Massen
comparing 4 different methods to compute sunshine duration from pyranometer |
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Biologically
eff. UVB dose on a horizontal plane in kWh/m2
Practically flat trend line for the whole period.
mean +/- stdev: Practically flat trend from 1998 to 2013, but See
[10]
and [22] (poster finds slight
positive trend in June (+2%) and negative trend in August (-1%), no trend
for other months, for period 1991 to 2008) |
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UVA
dose on a horizontal plane in kWh/m2 Positive trend: + 0.2 kWh*m-2*y-1, essentially caused by the suspiciously high 2010 reading. Negative trend of -30 Wh*m-2*y-1 since 2004, consistent with the pyranometer and UVB data.
mean +/- stdev: The 3 independent measures of Solar energy, UVA and UVB dose all document a solar dimming since 2004. |
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NO
concentration in ug/m3 The 1998-1999 data are too unreliable to be retained. 2000 to 2013: trend: - 0.3 ug*m-3*y-1 see [11] which gives ~30% reduction from 1990 to 2005 for the EU-15 countries. |
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NO2
concentration in ug/m3
The 1998-1999 data are too unreliable to be retained. 2000 to 2013: trend: + 0.3 ug*m-3*y-1 Many missing data from 2011 to 2013 ( 25%, 21% , 8%) so be careful! All these concentrations are low! Luxembourg-City has a background of 58 and rural Vianden (Niklausberg) one of 9.4 (average since 1988) [38]
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Enthalpy of moist air in kJ/kg See [24] on how the energy content of moist air is
calculated. Several authors, as Prof. Roger Pielke Sr. insist that air
temperature is a poor metric for global warming/cooling, and that the energy
content of the moist air and/or the Ocean Heat Content (OHC) are better. |
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References:
1 | Europe's Environment 4th AR (2007) Fig. 2.2.3 http://reports.eea.europa.eu/state_of_environment_report_2007_1/en/Belgrade_EN_all_chapters_incl_cover.pdf |
2 | EPA: Ozone trends. http://www.epa.gov/airtrends/ozone.html |
3 |
Jonson et al: Can we explain the trends in European ozone levels? Atmos. Chem. Phys. Discuss., 5, 5957–5985, 2005. http://www.atmos-chem-phys-discuss.net/5/5957/2005/acpd-5-5957-2005.pdf |
4 | Ozone trends at Uccle http://ozone.meteo.be/ozone/trends.php |
5 | Rebetez, Beniston: Analyses of the elevation dependency of correlations between sunshine duration and diurnal temperature range this century in the Swiss Alps. 1998. |
6 | R.G. Vines, CSIRO: European rainfall patterns. International Journal of Climatology, vol.5, issue 6, p. 607-616. |
7 | http://global-warming.accuweather.com (15 Jan 2009). |
8 | J.W. Krzyscin, J.L.Borkowski: Total ozone trend over Europe: 1950 - 2004. ACPD, 8, 47-69, 2008. |
9 | NASA: Solar Physics: The Sunspot Cycle. |
10 | de Backer et al: ftp://ftp.kmi.be/dist/meteo/hugo/posters/20080630tromso_hdb.pdf (temporarly unavailable) |
11 | EEA: Emission trends of NOx 1990 - 2005 |
12 | L. Motl: http://motls.blogspot.com/2009/12/uah-msu-temperatures-for-2009-and.html . Dec.2009 |
13 | K. Makovski: The daily temperature amplitude and surface solar radiation..Dissertation for the degree of doctor of sciences. ETHZ 2009. |
14 | A. Ohmura: Observed long-term variations of solar irradiance at the earth's surface. Space Science Reviews (2006) 125: 111-128 |
15 | J. van Oldenvorgh: Western Europe is warming much faster than expected. Clim.Past. 16Jan.2009 |
16 | Van Malderen, De Backer, Delcloo: Revision of 40 years of ozone measurements in Uccle, Belgium. Poster, EGU2009, Vienna. |
17 | EEA: Air pollution by ozone across Europe during summer 2009 |
18 | Climate4 you: Global temperature trends |
19 | Lindzen & Choi: On the determination of climate feedback from ERBE data (GRL, 2009) |
20 | Scafetta, N.: Empirical analysis of the solar contribution to global mean air surface temperature change. Journal of Atmospheric and Solar-Terrestrial Physics, 2009 (doi:10.1016/j.jastp.2009.07.007) |
21 |
Massen, F., Beck, E. :Accurate
estimation of CO2 background level from near ground
measurements at non-mixed environments
in: Leal, W., editor: The Economic, Social and
Political Elements of Climate Change
Climate Change Management, 2011, Part 4,
509-522. Springer.
DOI:
10.1007/978-3-642-14776-0_31
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22 | De Backer & Van Malderen: Time series of daily erythemal UVB doses at Uccle Belgium. Poster, July 2009. |
23 | Massen, F.: Sunshine duration from pyranometer readings, 2011 |
24 | Massen F., Calculating moist enthalpy from usual meteorological measurements (July 2010) and Calculating moist enthalpy revisited (Sep. 2010) |
25 | CDIAC: Online Trends |
26 | UAH MSU data: http://vortex.nsstc.uah.edu/public/msu/ |
27 | Vigouroux et al: Evaluation of ozone trends from g-b FTIR observations. Atmos. Chem. Phys., 8, 6865–6886, 2008 |
28 |
UNEP, Scientific Assessment: Stratospheric Ozone and
Surface Ultraviolet Radiation http://ozone.unep.org/Assessment_Panels/SAP/Scientific_Assessment_2010/04-Chapter_2.pdf |
29 | http://berkeleyearth.lbl.gov/regions/luxembourg |
30 | K. Makowski: The daily temperature amplitude and surface solar radiation. Dissertation ETH Zürich #18319, 2009 |
31 | http://de.wikipedia.org/wiki/Zeitreihe_der_Lufttemperatur_in_Deutschland#Winter |
32 | Tim Osborne: NAO data (http://www.cru.uea.ac.uk/~timo/datapages/naoi.htm) |
33 | Helioclim satellite measurements of solar irradiation at http://www.soda-is.com/eng/services/services_radiation_free_eng.php |
34 | http://www.esrl.noaa.gov/gmd/ |
35 | http://www.atmos.ucla.edu/~qli/publications/Jiang_2011_GBC.pdf |
36 | Fung: A Hyperventilationg Biosphere (Sep. 2013) |
37 |
Fraunhofer Institut Stromproduktion : http://www.ise.fraunhofer.de/de/downloads/pdf-files/aktuelles/stromproduktion-aus-solar-und-windenergie-2013.pdf |
38 | EEA interacive map. http://www.eea.europa.eu/themes/air/interactive/no2 |
39 | Portail de l'Evironnement: http://www.environnement.public.lu/air_bruit/dossiers/PA-reseaux_mesure_air/reseau_automatique/resultats_mesures_live/index.html |
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Addendum
1 updated! |
Lindzen & Choi [19] define the non-feedback
climate sensitivity as ΔT0 = G0*ΔQ, where G0
= 0.25 Wm-2 and ΔQ is the change in radiative forcing.
A change of -2.6 kWh*m-2y-1 (period 2004 to
2013) corresponds to ΔQ
= - 2600/8760 = -0.297 Wm-2 and should yield a cooling of ΔT0
= -0.25*0.297 = -0.84 K (or °C).per year. Scafetta [20] defines a climate sensitivity in respect to changes in solar radiation by k1s = ΔT/ΔF and finds k1s = 0.053. Our data for the full period 2004 to 2013 give ΔT/ΔF= - 0.0154/(-0.297) = 0.052, a value practically identical to that of Scafetta!. Summary for the 2004 to 2013 period:
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Addendum
2 (to be updated!) |
It makes for an interesting exercise to compare
the influence of mean yearly solar forcing on moist enthalpy and air
temperature for the decade 2002 to 2011.
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file: meteolcd_trends.html
francis.massen@education.lu
last revision: 07 Feb 2014