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首页> 外文期刊>ournal of the Meteorological Society of Japan >Numerical Investigation of Climate Factors Impact on Carbon Cycle in the East Asian Terrestrial Ecosystem
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Numerical Investigation of Climate Factors Impact on Carbon Cycle in the East Asian Terrestrial Ecosystem

机译:气候因素对东亚陆地生态系统碳循环影响的数值研究

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摘要

Using a regional climate model that includes a terrestrial biosphere model, numerical simulations were performed to clarify the mechanism of the carbon cycle between the terrestrial ecosystem and the atmosphere and to investigate the climate factors impact on the carbon cycle in the East Asian terrestrial ecosystem.Model verifications were performed with regard to the principal elements: precipitation and vegetation phenology. The variations of the atmospheric carbon dioxide concentration simulated by the model were validated using the data at six in situ observatories.After the confirmations of the model performance, regional features of the impact of climate factors on the gross primary production (GPP) were analyzed. The downward short-wave radiation (DSW), the soil wetness (SW), and the surface temperature (TA) were chosen as the effective climate factors. In the NE-Asia region, a positive anomaly of DSW in warm season induces a positive anomaly of GPP. High anomalous TA in the cold season also induces a large value of GPP. In the China region, similarly to that in NE-Asia, DSW is important for GPP. The effect of SW is also important in the spring. While the correlation between the variation of TA and that of GPP is positive and high in winter, the positive anomaly of TA in the warm season induces negative anomaly of GPP. In the Indochina region, DSW is important throughout the year. In contrast, the correlations between the variations of SW and those of GPP are negative in all seasons, indicating that GPP becomes a negative anomaly when the precipitation is a positive anomaly. In the India region, DSW in the warm season and SW in the cold season are important for increasing GPP. In the Mongolia and Inland regions, SW is a more important climate factor than DSW for GPP. High temperature in the cold season is also important. In summer, unusually high temperature and dry climate conditions reduce GPP. In the Philippines region, main factor affecting GPP is DSW.
机译:使用包括陆地生物圈模型在内的区域气候模型,进行了数值模拟,以弄清陆地生态系统与大气之间的碳循环机制,并研究气候因素对东亚陆地生态系统碳循环的影响。关于主要要素进行了验证:降水和植被物候。利用六个现场观测站的数据验证了该模型模拟的大气中二氧化碳浓度的变化。在确认模型性能之后,分析了气候因素对初级总产值(GPP)影响的区域特征。选择向下的短波辐射(DSW),土壤湿度(SW)和地表温度(TA)作为有效的气候因子。在东北亚地区,温暖季节DSW的正异常引起GPP的正异常。寒冷季节的高TA异常也诱发了很大的GPP值。在中国地区,与NE-Asia相似,DSW对于GPP也很重要。在春季,SW的作用也很重要。虽然TA和GPP的变化之间的相关在冬季是正的且较高,但在温暖季节TA的正异常会导致GPP的负异常。在印度支那地区,DSW全年都很重要。相反,SW的变化与GPP的变化之间的相关性在所有季节均为负,表明当降水为正异常时,GPP变为负异常。在印度地区,暖季的DSW和冷季的SW对于增加GPP很重要。在蒙古和内陆地区,与GPP的DSW相比,SW是更重要的气候因子。寒冷季节的高温也很重要。在夏季,异常高温和干旱气候条件会降低GPP。在菲律宾地区,影响GPP的主要因素是DSW。

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