منابع مشابه
Regimes of the North Australian Wet Season
The variability of the north Australian wet season is examined by performing cluster analysis on the wind and thermodynamic information contained in the 2300 UTC radiosonde data at Darwin for 49 wet seasons (September–April) from 1957/58 to 2005/06. Five objectively derived regimes of the wet season are obtained and are found to differ significantly in their synoptic environment, cloud patterns...
متن کاملTrends in the start of the wet season over Africa
A quarter of a century of daily rainfall data from the Global Telecommunications System are used to define the temporal and spatial variability of the start of the wet season over Africa and surrounding extreme south of Europe and parts of the Middle East. From 1978 to 2002, the start of the wet season arrived later in the year for the majority of the region, as time progressed. In some parts o...
متن کاملRainforest-initiated wet season onset over the southern Amazon.
Although it is well established that transpiration contributes much of the water for rainfall over Amazonia, it remains unclear whether transpiration helps to drive or merely responds to the seasonal cycle of rainfall. Here, we use multiple independent satellite datasets to show that rainforest transpiration enables an increase of shallow convection that moistens and destabilizes the atmosphere...
متن کاملWet-season spatial variability of `="0200`="003DN2O emissions
Introduction Conclusions References
متن کاملInfluence of Wet and Dry Season on Milk Composition of Dromedary Camels (Camelus dromedarius) from Tunisia
This study investigated the effect of season (wet and dry) on milk composition of the dromedary camel (Camelus dromedarius). Milk samples representing the wet and dry seasons were analyzed for total solids (TS), fat (F), solids-non-fat (SNF), ash, crude protein (CP), nitrogen soluble at pH 4.6 (SN), mineral content (MC) and casein fraction (CnF). Camel milk had higher (P
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ژورنال
عنوان ژورنال: Nature Climate Change
سال: 2019
ISSN: 1758-678X,1758-6798
DOI: 10.1038/s41558-019-0495-8