We formulate six processes that may explain why the largest losses are observed specifically over concentrated brines and/or exposed sediments. High temperatures and alkalinity are known to promote NH 3 losses from soda lakes. The likely source of NH 3 at Lake Natron is decomposition of organic material, either from rivers and springs or produced in the lake (plankton, bird excreta). The timing is different from the agricultural dominated NH 3 emissions in the wider Natron area, which peak early in the year, after the first wet season. The largest NH 3 column loadings generally occur at the end of the dry season in September–November over Lake Natron’s largest mudflat, that is exposed with receding water levels. ![]() Temporal analysis reveals that the emissions are episodic and linked with the lake’s surface area. Here we explore 10 years of IASI NH 3 satellite data and other publicly available datasets over the area to characterize the natural NH 3 emissions in this unique ecosystem. ![]() Its remote location and the absence of nearby large anthropogenic sources suggest that the observed NH 3 is mainly of natural origin. The lake is in the centre of an endorheic (limited drainage) basin and has shallow, saline-alkaline waters. In a recent global analysis of satellite-derived atmospheric NH 3 data, a hotspot was observed in the vicinity of Lake Natron, Tanzania.
0 Comments
Leave a Reply. |