Evaluation and simulation of terrestrial latent heat flux globally: A collaborative effort utilizing CMIP6 climate models and eddy covariance observations

IF 5.6 1区 农林科学 Q1 AGRONOMY Agricultural and Forest Meteorology Pub Date : 2024-12-21 DOI:10.1016/j.agrformet.2024.110371
Xinling Tian, Zhenhua Di, Yunjun Yao, Zhenwei Liu, Hao Meng, Huiying Sun, Xueyan Wang, Wenjuan Zhang
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Abstract

Exchanging latent heat flux (LE) through evapotranspiration impacts the atmospheric thermodynamics and water cycle. The Earth System Models (ESMs) in the Coupled Model Intercomparison Project Phase6 (CMIP6) are vital to reproduce improved LE variations globally, albeit with significant uncertainties. Meanwhile, the rational attribution to regions of LE simulations is essential for informed water resources administration and climate control. This paper presents the first comprehensive evaluation of the ability of 49 ESMs to model global terrestrial LE during the 2000–2014 period based on 205 eddy covariance (EC) observations. Utilizing the Bayesian Model Averaging (BMA) method, we analyzed the spatial-temporal variation and attribution to regions of global LE during 1980–2014 by combining the top six models with EC observations. The results showed that most ESMs overestimated LE, with an average BIAS of 7.57 W‧m−2, covering −7–17 W‧m−2. Among them, the MIROC6 model evinced the highest predictive skill at various land cover types. Moreover, the BMA-based global average terrestrial LE showed low LE values in dry and cold regions of temperate and cold zones of middle and high latitudes but evidenced high LE values in hot and humid regions of low-latitude tropical zones. The inter-annual variations of the BMA-based global annual LE exhibited a significant linear increasing trend with a 0.027 W‧m−2 slope (P-value <0.05). Further attribution to regions analyses were concluded, considering that LE trends were the same as the temperature trends in the Northern Hemisphere, especially in the middle and high latitudes. These conditions are comparable to radiation in the equatorial regions, correlating substantially with precipitation in dry and semi-dry regions across Asia, Europe, and Africa. In addition, the advantages of CMIP6 ESMs on LE simulations mainly including bias, and interannual variability characteristics were also concluded compared with CMIP5 ESMs.
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全球陆地潜热通量的评估和模拟:基于CMIP6气候模式和涡旋相关方差观测的协同努力
通过蒸散发交换潜热通量影响大气热力学和水循环。耦合模式比对项目第6阶段(CMIP6)中的地球系统模式(esm)对于重现全球LE变化的改善至关重要,尽管存在很大的不确定性。同时,LE模拟的合理区域归属对水资源管理和气候控制具有重要意义。本文首次综合评价了49个esm在2000-2014年期间基于205个涡动相关(eddy covariance, EC)观测数据模拟全球陆地LE的能力。利用贝叶斯模式平均(BMA)方法,结合前6个模式和EC观测数据,分析了1980—2014年全球LE的时空变化及其区域归因。结果表明,大多数esm高估了LE,平均BIAS为7.57 W·m−2,覆盖了- 7 ~ 17 W·m−2。其中,MIROC6模式对不同土地覆盖类型的预测能力最高。此外,基于bma的全球平均陆地LE在中高纬度温带和寒带的干燥寒冷地区表现出较低的LE值,而在低纬度热带湿热地区表现出较高的LE值。基于bma的全球年LE年际变化呈显著的线性增加趋势,斜率为0.027 W·m−2 (p值<;0.05)。考虑到北半球特别是中高纬度地区的气温变化趋势与LE变化趋势一致,进一步将其归因于区域分析。这些条件与赤道地区的辐射相当,与亚洲、欧洲和非洲干旱和半干旱地区的降水密切相关。此外,对比CMIP5 ESMs, CMIP6 ESMs在LE模拟中的优势主要包括偏倚和年际变化特征。
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来源期刊
CiteScore
10.30
自引率
9.70%
发文量
415
审稿时长
69 days
期刊介绍: Agricultural and Forest Meteorology is an international journal for the publication of original articles and reviews on the inter-relationship between meteorology, agriculture, forestry, and natural ecosystems. Emphasis is on basic and applied scientific research relevant to practical problems in the field of plant and soil sciences, ecology and biogeochemistry as affected by weather as well as climate variability and change. Theoretical models should be tested against experimental data. Articles must appeal to an international audience. Special issues devoted to single topics are also published. Typical topics include canopy micrometeorology (e.g. canopy radiation transfer, turbulence near the ground, evapotranspiration, energy balance, fluxes of trace gases), micrometeorological instrumentation (e.g., sensors for trace gases, flux measurement instruments, radiation measurement techniques), aerobiology (e.g. the dispersion of pollen, spores, insects and pesticides), biometeorology (e.g. the effect of weather and climate on plant distribution, crop yield, water-use efficiency, and plant phenology), forest-fire/weather interactions, and feedbacks from vegetation to weather and the climate system.
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