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Evidence for a widespread climatic anomaly at around 9.2 ka before present

机译:目前存在大约9.2 ka的广泛气候异常的证据

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The 8.2 ka event was triggered by a meltwater pulse (MWP) into the North Atlantic and resultant reduction of the thermohaline circulation (THC). This event was preceded by a series of at least 14 MWPs; their impact on early Holocene climate has remained almost unknown. A set of high-quality paleoclimate records from across the Northern Hemisphere shows evidence for a widespread and significant climatic anomaly at similar to 9.2 ka B. P. This event has climatic anomaly patterns very similar to the 8.2 ka B. P. event, cooling occurred at high latitudes and midlatitudes and drying took place in the northern tropics, and is concurrent with an MWP of considerable volume (similar to 8100 km(3)). As the 9.2 ka MWP occurs at a time of enhanced baseline freshwater flow into the North Atlantic, this MWP may have been, despite its relatively small volume, sufficient to weaken THC and to induce the observed climate anomaly pattern.
机译:8.2 ka事件是由进入北大西洋的融水脉冲(MWP)以及由此导致的热盐环流(THC)减少引起的。在此事件之前,一系列至少14个MWP;它们对早期全新世气候的影响几乎未知。来自北半球的一组高质量的古气候记录显示,证据表明在9.2 ka BP附近出现了广泛且显着的气候异常。该事件的气候异常模式与8.2 ka BP事件非常相似,降温发生在高纬度和中纬度干燥发生在北热带地区,并伴随着相当大的MWP(类似于8100 km(3))。由于9.2 ka MWP发生在流入北大西洋的基线淡水增加时,尽管其MWP相对较小,但它可能足以削弱THC并诱发观测到的气候异常模式。

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