{"id":5800,"date":"2017-05-27T13:50:30","date_gmt":"2017-05-27T13:50:30","guid":{"rendered":"https:\/\/rsoftsolution.com\/blog\/increased-leaf-abundance-is-a-double-edged-sword.html"},"modified":"2017-05-27T13:50:30","modified_gmt":"2017-05-27T13:50:30","slug":"increased-leaf-abundance-is-a-double-edged-sword","status":"publish","type":"post","link":"https:\/\/www.rbsitsoftwaresolution.in\/blog\/increased-leaf-abundance-is-a-double-edged-sword.html","title":{"rendered":"Increased leaf abundance is a double-edged sword"},"content":{"rendered":"<p>A substantial portion of the planet is greening in response to increasing atmospheric carbon dioxide, nitrogen deposition, global warming and land use change. The increase in leafy green coverage, or leaf area index (<em>LAI<\/em>), will hold important implications for climate change feedback loops, yet quantifying these impacts on a global scale can be challenging. Here, Giovanni Forzieri and colleagues analyzed satellite data of global <em>LAI<\/em> coverage between 1982 and 2011.<\/p>\n<p>Their results varied depending on the local biome, where increased <em>LAI<\/em> in boreal regions caused a reduction in surface albedo (reflection of sunlight), and thus resulted in a warming effect; in contrast, increased <em>LAI<\/em> in arid regions caused an increase in transpiration, and thus drove a cooling effect.<\/p>\n<p>What&#8217;s more, the authors found that these relationships between <em>LAI<\/em> and surface biophysics were amplified up to five times under extreme warm-dry and cold-wet years.<\/p>\n<p>They estimate that, across about 60% of the global vegetated area, greening has buffered warming by about 14%; for the remaining areas, which mostly include boreal zones, <em>LAI<\/em> trends have amplified the raise in air temperatures, leading to an additional warming of about 10%.<\/p>\n<p>Article source: https:\/\/www.sciencedaily.com\/releases\/2017\/05\/170525141556.htm<\/p>","protected":false},"excerpt":{"rendered":"<p>A substantial portion of the planet is greening in response to increasing atmospheric carbon dioxide, nitrogen deposition, global warming and land use change. 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