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Hourly mean time series of external SHE coefficients in a geomagnetic dipole coordinate system (up to degree 3 and order 1) have been derived by analysis of 4.5 years of observatory data (July 1998-December 2002), details of the derivation are given in Olsen et al. (2005).
Neoorthosiphonone B (1) was found to have the molecular formula C38H44O11 (17° of unsaturation) derived by analysis of its HRESIMS at m/z 699.2798 [M+Na]+ (calcd for C38H44O11Na, 699.2776), 13C NMR, and DEPT spectra.
An external field model up to degree 3 and order 1 (in the geomagnetic coordinate system), and with 1 hr sampling interval was derived by analysis of 4.5 years of ground observatory hourly means from July 1998 to December 2002 (Olsen et al., 2005).
The limits for the visual grades are given in Table 3 and were derived by analysis of a subset of patients and reported in a previous study (Atkin et al, 2005).
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Definitions and examples of the types of challenges (derived by initial analysis and repeated re-analysis to refine the definitions) are explained in detail in the "Challenges faced and scaffolds required" section.
The tension of the mooring line was derived by hydrodynamic analysis using the de-coupled analysis method.
Surface structure of synthesized material was derived by FTIR analysis.
Firstly the governing dimensionless numbers are derived by dimensional analysis.
(a) Source and destination strength averaged for each of the five different provinces (derived by cluster analysis, Fig. S1).
Corresponding transmission conditions have been derived by asymptotic analysis.
The different colours denote each of the five different provinces, derived by cluster analysis on pairwise Mean Connection Time –MCT (days) (Supplementary Fig. S1).
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