## Abstract A substantial decrease in snow cover extent (SCE) and snow depth over North America has been observed over the 1960–2000 period. One explanation for the changes in North American snow cover is a change in the frequency and/or intensity of snow ablation. This study uses a gridded dataset
Observed trends in sunshine duration over South America
✍ Scribed by Carlos Raichijk
- Publisher
- John Wiley and Sons
- Year
- 2011
- Tongue
- English
- Weight
- 303 KB
- Volume
- 32
- Category
- Article
- ISSN
- 0899-8418
- DOI
- 10.1002/joc.2296
No coin nor oath required. For personal study only.
✦ Synopsis
Abstract
In this work, temporal series of monthly mean values of sunshine duration were studied in five climatic regions of South America. For this purpose, data from 237 meteorological stations throughout South America were taken into account in: Argentina (20), Bolivia (2), Brazil (190), Paraguay (11), Peru (3), and Uruguay (11). The stations have been grouped into the following five climatic regions according to the classification of the Brazilian Institute of Geography and Statistics (IBGE): Equatorial, Tropical Equatorial, Tropical Central Brazil—Warm, Tropical Central Brazil—Mesothermal, and Humid Temperate. The non‐parametric test of Mann‐Kendall was used to evaluate possible trends for both the period of maximum extension of available data, 1961–2004, as well as for the sub‐periods 1961–1990 and 1991–2004. From this analysis, significant trends could be observed, first decreasing between 1961 and 1990, and then increasing from 1990 onwards. The trends found for the regions studied are in agreement with those observed in other regions of the planet, thus providing further evidence of the phenomenon that has been referred to as global dimming and brightening. Copyright © 2011 Royal Meteorological Society
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