This research focuses on the Cambrian Mountains of Wales, UK, where lichenometric dating of geomorphological features and palaeohydrological reconstructions is combined with climatological data and documentary flood records.
As expected, many DInSAR values are close to the detection threshold (i.e., 1 cm) and therefore do not indicate significant change; however, DInSAR seasonal ground displacement patterns aligned well with climatological and soil conditions and offer geomorphological insight into subsurface processes in permafrost environments.
These results with post-sunset equatorial irregularities whose occurrence peak falls on the equinox and lowest values during solstices are in a proper agreement with climatological characteristics of the plasma bubbles occurrence in the topside ionosphere reported in previous studies (e.g., Burke et al. 2004; Su et al. 2006; Stolle et al. 2006; Park et al. 2013).
In order to represent the regular part of the observed P (LT, D, Y) behavior that we expect to be associated with climatological specifics of the diurnal, seasonal, and long-term solar activity variations, we used the 27-day sliding window median Pmed (LT, D, Y) for each combination of LT, D, and Y in the sets {P (LT, D 13, Y), ⋯, P (LT, D+13, Y}.
Hurricane Juan alerted residents, governments, utilities, and emergency management agencies throughout Atlantic Canada to improve preparations for devastating events such as hurricanes, especially with climatological data pointing to possible increased frequency of major ocean storms and extratropical cyclones.
The timing of local pandemic onset was not significantly correlated with climatological variables including minimum temperature (rho = 0.15, P = 0.62), maximum temperature (rho=−0.001, P=0.99), precipitation (rho = −0.3, P = 0.30), relative humidity (rho = −0.05, P = 0.89) and specific humidity (rho = −0.08, P = 0.80), after adjusting for population size.
Turbulent kinetic energy dissipation rates based on radar observations are presented and compared with corresponding climatological summer and winter profiles from rocket measurements, as well as with single profiles from model runs for selected periods from September 2003 to Summer 2004.
Here, we present the results for 2003 in comparison with the climatological means.
Design wind effects on tall buildings are estimated by combining aerodynamic data obtained from wind tunnel tests with the climatological or wind speed data of the construction site.
Three biometeorological indices were examined in terms of their potential to describe the actual thermal sensation as this is experienced by humans at areas with different climatological characteristics.
Full fields of standard error of the mean and observed minus analyzed difference are provided with the climatological mean fields of conductivity at https://www.nodc.noaa.gov/OC5/woa13/.
