Map climatic features as the long-term mean values (of atmospheric pressure, temperature, humidity, total precipitation, and so forth) to connect points with equal values of the feature in question—for example, isobars for pressure, isotherms for temperature, and isohyets for precipitation. Isoamplitudes are drawn on maps of amplitudes (for example, annual amplitudes of air temperature—that is, the differences between the mean temperatures of the warmest and coldest month). Isanomals are drawn on maps of anomalies (for example, deviations of the mean temperature of each place from the mean temperature of the entire latitudinal zone). Isolines of frequency are drawn on maps showing
Atmospheric-pressure laser ionization selectivity of APLI is one factor contributing to the selectivity, but under LC conditions, APPI suffers from another effect: The VUV light utilized by APPI does not penetrate deep into the ion source geometry, because the solvents used by LC, which are present as vapor in the ion source, strongly absorb the VUV light. For the UV light of APLI the LC solvents are virtually transparent, thus APLI allows the generation of ions in the entire ion source volume. In contrast to other ionization methods such as electrospray ionization (ESI) and atmospheric-pressure chemical ionization (APCI), APLI allows the generation of