Research Article

Six Temperature Proxies of Scots Pine from the Interior of Northern Fennoscandia Combined in Three Frequency Ranges

Table 1

Six proxies versus mean July temperatures (average of the four records, no filtering) in 1908–2002. Reduction of error (RE), coefficient of efficiency (CE), and during EC-LV (early calibration in 1908–1955 and late verification in 1955–2002) and LC-EV (late calibration in 1955–2002 and early verification in 1908–1955). Only test results with RE and CE > 0 are included.

EC-LVLC-EV
RECE RECE

(A) RCS indexing
 FXD0.290.210.350.100.020.14
 RRW0.250.170.190.210.140.16
(B) 180-year spline indexing
 SRW0.300.220.290.240.180.32
 SXD0.260.180.250.150.080.12
 FXD0.350.280.360.140.070.15
 RRW0.270.190.210.230.170.18
(C) 30-year spline indexing
 SRW0.270.190.300.40.340.43
 FRW0.290.210.390.130.050.24
 FHI0.520.470.570.230.170.23
 RRW0.180.090.250.270.200.33