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A high‐quality daily runoff time series of the Lake Como inflow and outflow, the longest for Italian Alps, was reconstructed for the 1845–2016 period in the Adda river basin. It was compared with contemporary monthly precipitation and temperature observations and estimated potential evapotranspiration losses. Trend analyses were conducted for daily flow maxima and 7‐day duration minima of inflows into the lake showing a non‐significant decrease and a significant increase, respectively. Although the annual precipitation time series exhibits a non‐significant decrease, annual runoff volumes decrease with a rate of −136 mm⋅century−1, with a significance level of 5%. Possible causes of variability of rainfall and runoff as North Atlantic Oscillation (NAO), Atlantic Multidecadal Oscillation and Western Mediterranean Oscillation indexes and sunspot activity were also explored. Wavelet spectra analyses of monthly precipitation and runoff show some changes in the energy both at small and large scales and are effective in pointing out phenomena as droughts and the effects of dams' regulation. Conversely, wavelet coherence spectra indicate a weak correlation of NAO and sunspots with precipitation. In addition, the analysis of temperature and potential evapotranspiration tendencies suggests that the decrease of runoff has to be ascribed mostly to anthropogenic factors, including water abstraction for irrigation and increased evapotranspiration losses due to natural afforestation and, only in part, to climatic variability. [ABSTRACT FROM AUTHOR]

From the origins of hydrology, the time of concentration, tc, has conventionally been tackled as a constant quantity. However, theoretical proof and empirical evidence imply that tc exhibits significant variability against rainfall, making its definition and estimation a hydrological paradox. Adopting the assumptions of the Rational method and the kinematic approach, an effective procedure in a GIS environment for estimating the travel time across a catchment’s longest flow path is provided. By application in 30 Mediterranean basins, it is illustrated that tc is a negative power function of excess rainfall intensity. Regional formulas are established to infer its multiplier (unit time of concentration) and exponent from abstract geomorphological information, which are validated against observed data and theoretical literature outcomes. Besides offering a fast and easy solution to the paradox, we highlight the necessity of implementing the varying tc concept within hydrological modelling, signalling a major shift from current engineering practices. [ABSTRACT FROM AUTHOR]

Cervical lymphadenopathy (CL) is common in childhood. The aim of this study is to evaluate the etiology, follow-up, and treatment of persistent CL. The authors studied retrospectively 50 children with CL, hospitalized at the Department of Pediatrics and Pediatrics Surgery. Patients underwent ultrasonography. Thirty-six percent presented abnormal ultrasonographic image and underwent excisional biopsy. Biopsies revealed 4 thyroglossal cysts, 3 branchial cysts, 1 hemangioma, 2 sebaceous cysts, 1 dermoid cyst, 5 occurrences of tuberculosis lymphadenitis, 1 occurrence of Bartonella henselae lymphadenopathy, and 1 case of non-Hodgkin lymphoma. In conclusion, CL is usually a benign finding; bacterial and viral infections are the most common causes. Ultrasonography help in etiology and follow-up of CL. [ABSTRACT FROM AUTHOR]