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What could have caused pre-industrial biomass burning emissions to exceed current rates?

机译:是什么导致工业化之前的生物质燃烧排放量超过当前水平?

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Recent studies based on trace gas mixing ratios in ice cores and charcoaldata indicate that biomass burning emissions over the past millenniumexceeded contemporary emissions by up to a factor of 4 for certain timeperiods. This is surprising because various sources of biomass burning arelinked with population density, which has increased over the past centuries.We have analysed how emissions from several landscape biomass burning sourcescould have fluctuated to yield emissions that are in correspondence withrecent results based on ice core mixing ratios of carbon monoxide (CO) andits isotopic signature measured at South Pole station (SPO). Based onestimates of contemporary landscape fire emissions and the TM5 chemicaltransport model driven by present-day atmospheric transport and OHconcentrations, we found that CO mixing ratios at SPO are more sensitive toemissions from South America and Australia than from Africa, and arerelatively insensitive to emissions from the Northern Hemisphere. We thenexplored how various landscape biomass burning sources may have varied overthe past centuries and what the resulting emissions and corresponding COmixing ratio at SPO would be, using population density variations toreconstruct sources driven by humans (e.g., fuelwood burning) and a new modelto relate savanna emissions to changes in fire return times. We found that tomatch the observed ice core CO data, all savannas in the Southern Hemispherehad to burn annually, or bi-annually in combination with deforestation andslash and burn agriculture exceeding current levels, despite much lowerpopulation densities and lack of machinery to aid the deforestation process.While possible, these scenarios are unlikely and in conflict with currentliterature. However, we do show the large potential for increasedemissions from savannas in a pre-industrial world. This is mainlybecause in the past, fuel beds were probably less fragmented compared to thecurrent situation; satellite data indicates that the majority of savannashave not burned in the past 10 yr, even in Africa, which is considered "theburning continent". Although we have not considered increased charcoalburning or changes in OH concentrations as potential causes for the elevatedCO concentrations found at SPO, it is unlikely they can explain the largeincrease found in the CO concentrations in ice core data. Confirmation of theCO ice core data would therefore call for radical new thinking about causesof variable global fire rates over recent centuries.
机译:基于冰芯和木炭数据中痕量气体混合比的最新研究表明,在过去的千年中,在一定时期内,燃烧生物质的排放量超过了现代排放量的4倍。这是令人惊讶的,因为各种生物质燃烧的源头与人口密度相关联,而人口密度在过去几个世纪中一直在增加。一氧化碳(CO)及其同位素标记在南极站(SPO)进行了测量。根据当代景观火排放的估算值以及由当今大气传输和OH浓度驱动的TM5化学传输模型,我们发现SPO的CO混合比对来自南美和澳大利亚的排放比对来自非洲的排放更敏感,并且对来自SPO的排放不敏感。北半球。然后,我们使用人口密度变化来重构人类驱动的来源(例如薪柴燃烧)和一种新的模型来关联热带稀树草原的排放,探讨了过去几个世纪以来各种景观生物质燃烧源可能如何变化,以及在SPO处产生的排放量和相应的COmi​​xing比如何。改变回火时间。我们发现,为了匹配观测到的冰芯CO数据,南半球的所有稀树草原必须每年或每两年烧毁一次,再加上砍伐森林和砍伐森林,烧毁农业超过当前水平,尽管人口密度低得多,并且缺乏帮助毁林过程的机械尽管可能,但这些情况不太可能发生,并且与当前文学相冲突。但是,我们的确显示了在工业化前世界中稀树草原排放增加的巨大潜力。这主要是因为过去,与当前情况相比,燃料床的碎片化程度可能较小;卫星数据表明,即使在被视为“燃烧大陆”的非洲,也没有在过去10年中燃烧过大部分大草原。尽管我们尚未将炭燃烧增加或OH浓度变化视为SPO处CO浓度升高的潜在原因,但他们不太可能解释冰芯数据中CO浓度的大幅增加。因此,对CO冰芯数据的确认将需要对近几个世纪以来全球起火率变化的原因进行彻底的新思考。

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