Data trends at meteoLCD: 1998 to 2012
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 2012. http://meteo.lcd.lu
Older trends are here!
Most important conclusions (14 Apr 2013):
1. Solar dimming is happening at least since 2004 (Helioclim
satellite: since 1985)
2. Local temperatures are declining
3. There is no trend in DTR, daily max. and daily min. temperatures
4. The winters are cooling by 0.43 °C/decade
5. Ozone concentrations change for the better: ground O3 declines,
thickness of ozone layer increases
6. Long-term local CO2 mixing ratio increases by ~1.4 ppmV per year
Ground
Ozone [ug/m3] ("bad ozone") negative trend: -1.1 ug/m3 per year 1998-2012 mean
+/- stdev:
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Total
Ozone Column [DU] ("good ozone") positive trend: +2.1 DU per year, +0.3 since 2002 (Uccle gives +0.95 for the 1998-2010 period) (see also [16]) Calibration factors applied: 1998 to 2007: * 0.95 2008 to 2010: * 1.00 2011 : * 1.06 2012 : * 1.04 2012 common days measurements results: Diekirch = 325.6 DU Uccle DS = 328.1 DU Uccle data are from WOUDC (stat.53, Brewer#16) 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. 2002 to 2011 mean
+/- stdev:: 2007 to 2011:
See also [25] |
|
Air
temperature [°C]
Trend from 1998 to 2012: +0.019 °C per year 1998 to 2012 mean
+/- stdev::
2002 to 2011: The sensor has
not been moved since 2002! |
|
Diurnal
Temperature Range (DTR) [°C] DTR = daily max - daily min temperature 1998 to 2012 mean
+/- stdev:: |
. |
Winter
temperatures [°C]
Contrary to what is often suggested in the media, winters are cooling since 2002. The cooling rates per decade are: Diekirch: -0.43 °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] |
|
Total
Yearly Rainfall [mm]
Trend from 1998 to 2012: - 17 mm per year
1998 to 2012 mean +/- stdev::mean :
[6] gives medium term periods of 10 to12 years for the region from England to eastern Germany. |
|
Solar
energy on a horizontal plane mean: 1113.5 kWhm-2 |
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Sunshine
duration (derived from pyranometer data by Olivieri's method)
Total for 2012: 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.
1998 to 2012
mean +/-
stdev: Practically flat trend from 1998 to 2012, 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) |
|
UVA
dose on a horizontal plane in kWh/m2
Positive trend: + 0.3 k Whm-2 per year, essentially caused by the very low 2004 reading.
1998 to 2012
mean +/-
stdev:
Note
exceptional high 2010 reading causing a small positive trend of +0.15 kWm-2y-1
. This positive trend is caused by the exceptional high 2010 value (which
was an extrapolation due to 8% missing data, and is dubious). The 3 independent measures of Solar energy, UVA and UVB dose all document a solar dimming since 2004. |
|
NO
concentration in ug/m3 The 1998-1999 data are too unreliable to be retained. 2000 to 2012: trend = -0.3 ug/m3 per year see [11] which gives ~30% reduction from 1990 to 2005 for the EU-15 countries. |
|
NO2
concentration in ug/m3
The 1998-1999 data are too unreliable to be retained. 2000 to 2012: trend: - 0.014 ug/m3 per year
~ flat! Many (about 20 to 25%) missing data in 2011 and 2012, so be careful!
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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. |
|
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
|
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 |
R. Müller et al:
A New Estimate of the Average Earth Surface Land Temperature Spanning
1753 to 2011. GIGS, vol.1, nr.1 Jan.2013 |
30 | K. Makowski: The daily temperature amplitude and surface solar radiation. Dissertation ETH Zürich #18319, 2009 |
31 | http://notrickszone.com/2013/02/12/germanys-winter-temperature-trend-in-a-nosedive-now-falling-6c-per-century/ |
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 |
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 -1.5 kWh*m-2y-1 (period 2005 to
2012) corresponds to ΔQ
= - 1500/8760 = -0.171 Wm-2 and should yield a cooling of ΔT0
= -0.25*0.171 = -0.04 K (or °C).per year. Scafetta 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 2005 to 2012 give ΔT/ΔF= - 0.021/(-0.171) = 0.12. Summary for the 2005 to 2012 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: 14 Apr 13