System Nordsee
253
List of Figures
Atmospheric Physics
Fig. 2-1: NAO Index 2005. Ik: Ponta Delgada & Akureyri (Loewe and Koslowski 1998), Ipf6(lk):
low-pass filtered (6 month), cruuea: Gibraltar & Southwest Island, cpccdb: Amplitude of NAO
pattern from rotated principal component analysis of500 hPa height anomalies 38
Fig. 2-2: NAO phase portrait as percent freguency distribution of monthly dynamic NAO states
since 1879. Contours 0.5, 1, 1.5 and 2% are lines of egual relative state density (i.e. rel. #of
states per sguare-bin, 0.6 x 0.6). The seguences of 12 yellow and 12 blue circles (1,2,..., 8, 9,
O, N, D) show the temporal evolution in 2005 of raw (yellow) and low-pass filtered (6 month,
blue) monthly mean states, respectively. 40
Fig. 2-3: Sea level pressure (hPa) for the severe W-gale of Jan, 2 2005 together with grid posi
tions of weather-typing scheme 42
Fig. 2-4: Percent freguency distribution of daily circulation states for the period 1971 - 2000 to
gether with classification criteria 43
Fig. 2-5: Air circulation around high (A) and low pressure systems (C) 44
Fig. 2-6: Seasonal freguencies of reduced weather types in 2005 along with percentiles of empir
ical distributions for 1971 - 2000 (stacked columns); percentile range: 1 - 99, internal interval
limits at 5,25,50 (median), 75,95% 48
Fig. 2-7: As Fig. 2-6, except for monthly freguencies 49
Fig. 2-8: Classified seasonal sea level pressure distributions (hPa). Left: climatology (1971 -
2000), middle: 2005, right: anomalies; 1 = Winter = January, February, March etc. 52
Fig. 2-9: Monthly climatology of sea level pressure (hPa), base period 1971 - 2000 53
Fig. 2-10: Mon thly sea level pressure distributions (hPa) in 2005 55
Fig. 2-11: Monthly SLP-anomalies (hPa) in 2005 56
Fig. 2-12: Seasonal 50% probability ellipses for the >North Sea Wind< (1 = winter = JFM, 2 =
spring, etc.); top: 2005, bottom: 2004 59
Fig. 2-13: Progressive daily vectors of the >North Sea Wind< with ensemble and climatology.
Markers indicate the first day in a month, years final points of ensemble members 61
Fig. 2-14: Freguency of gale types G, SG,andVSG in days (stacked) in DJF win ter and win ter NAO
index. The correlation between total gale freguency and NAO index amounts to 0.71 65
Fig. 2-15: Total gale freguency (C+SC+ VSG) in days from October through March. Years refer to
JFM (OND from previous year, respectively). Right panel (fGales): lowpass filtered in yr-direc-
tion (filter length 5 yrs) 66
Fig. 2-16: Total gale freguency in fall, winter, and from October through March. Raw series (stip
pled) and overall linear trends (green, ±95% confidence interval) are shown along with low-
pass filtered series for filter lengths of 5 (blue) and 18 yrs (red, Ipl8). Stars mark break points
of piecewise linear trends fitted to Ipl8; accounted variances (R 2 ) refer to raw series 68
Fig. 2-17: Freguency ratio of severe and very severe gale days (SC+VSC) to total gale days (G+
SG+VSG). Otherwise as Fig. 2-16 69
Fig. 2-18: Seasonal cycle in 2005 of monthly averaged daily global radiation totals at Norder-
ney together with intramonthly extremes, 1971 -2000 base period monthly means, and
95%-band (climatology ± 1.96 standard deviations). 1 Idem 2 is eguivalent to a radiation
flux density of 116 Wm 2 . Raw data: Deutscher Wetterdienst. 71
Fig. 2-19: Monthly air surface temperatures at Norderney for 2005 together with 1971 - 2000
base period means, and 95%-band (climatology ± 1.96 standard deviations) 72