Temperature sensitivity of soil respiration is essential to predict possible changes in terrestrial carbon budget on various scenarios about atmospheric and soil climates. Although it is often evaluated by using respi...Temperature sensitivity of soil respiration is essential to predict possible changes in terrestrial carbon budget on various scenarios about atmospheric and soil climates. Although it is often evaluated by using respiratory quotient “Q<sub>10</sub>”, Q<sub>10</sub> values of soil respiration seem to vary depending on methods or scales of evaluation. Aiming at probing how Q<sub>10</sub> values of soil respiration are evaluated differently for a field, this study used a model of soil respiration rate, and numerically evaluated soil respiration rates along depth by fitting the model to depth distributions of CO<sub>2</sub> concentration measured in a field. And temperature sensitivity of soil respiration rate was evaluated by comparing the determined soil respiration rates with atmospheric and soil temperatures measured in the field. The results showed that the relation between surface CO<sub>2</sub> emission rates and atmospheric temperatures was represented by lower Q<sub>10</sub> values than that between soil respiration rates and soil temperatures, presumably because the top soil layers had acclimatized in more extent to the existing thermal regime than the underlying deeper layers. Thus, for evaluating effects of long-term rise in atmospheric temperature on soil respiration, it is necessary to precisely predict the long-term change in depth distribution of soil temperature as well as to quantify temperature sensitivity of soil respiration along depth. The evaluated sensitivity of surface CO<sub>2</sub> emission rate to atmospheric temperature showed hysteresis, implying the needs for more knowledge about temperature sensitivity of soil respiration evaluated in both warming and cooling processes for better understandings and predictions about terrestrial carbon cycling.展开更多
2022年4月10—14日浙江沿海海面出现一次持续时间长、范围广、浓度大的海雾过程。利用卫星资料、欧洲中期天气预报中心(European Centre for Medium-Range Weather Forecasts,ECMWF)发布的ERA-Interim(ECMWF Reanalysis-Interim)资料和...2022年4月10—14日浙江沿海海面出现一次持续时间长、范围广、浓度大的海雾过程。利用卫星资料、欧洲中期天气预报中心(European Centre for Medium-Range Weather Forecasts,ECMWF)发布的ERA-Interim(ECMWF Reanalysis-Interim)资料和浙江沿海自动气象观测站资料,分析此次过程的特征和成因。结果表明,低层逆温层使得低层水汽不易扩散到高空,有利于大雾的生成和维持。成雾阶段,有明显的水汽辐合,同时气温高于海面温度且差值为0~2.0℃。海雾维持且浓度较大时,水汽辐合逐渐减弱;气海温差(2 m气温减海面温度)则在0℃左右。消散阶段,有明显的水汽辐散;气海温差大于2.0℃或小于0℃。展开更多
文摘Temperature sensitivity of soil respiration is essential to predict possible changes in terrestrial carbon budget on various scenarios about atmospheric and soil climates. Although it is often evaluated by using respiratory quotient “Q<sub>10</sub>”, Q<sub>10</sub> values of soil respiration seem to vary depending on methods or scales of evaluation. Aiming at probing how Q<sub>10</sub> values of soil respiration are evaluated differently for a field, this study used a model of soil respiration rate, and numerically evaluated soil respiration rates along depth by fitting the model to depth distributions of CO<sub>2</sub> concentration measured in a field. And temperature sensitivity of soil respiration rate was evaluated by comparing the determined soil respiration rates with atmospheric and soil temperatures measured in the field. The results showed that the relation between surface CO<sub>2</sub> emission rates and atmospheric temperatures was represented by lower Q<sub>10</sub> values than that between soil respiration rates and soil temperatures, presumably because the top soil layers had acclimatized in more extent to the existing thermal regime than the underlying deeper layers. Thus, for evaluating effects of long-term rise in atmospheric temperature on soil respiration, it is necessary to precisely predict the long-term change in depth distribution of soil temperature as well as to quantify temperature sensitivity of soil respiration along depth. The evaluated sensitivity of surface CO<sub>2</sub> emission rate to atmospheric temperature showed hysteresis, implying the needs for more knowledge about temperature sensitivity of soil respiration evaluated in both warming and cooling processes for better understandings and predictions about terrestrial carbon cycling.
文摘2022年4月10—14日浙江沿海海面出现一次持续时间长、范围广、浓度大的海雾过程。利用卫星资料、欧洲中期天气预报中心(European Centre for Medium-Range Weather Forecasts,ECMWF)发布的ERA-Interim(ECMWF Reanalysis-Interim)资料和浙江沿海自动气象观测站资料,分析此次过程的特征和成因。结果表明,低层逆温层使得低层水汽不易扩散到高空,有利于大雾的生成和维持。成雾阶段,有明显的水汽辐合,同时气温高于海面温度且差值为0~2.0℃。海雾维持且浓度较大时,水汽辐合逐渐减弱;气海温差(2 m气温减海面温度)则在0℃左右。消散阶段,有明显的水汽辐散;气海温差大于2.0℃或小于0℃。
