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Determining lake surface water temperatures worldwide using a tuned one-dimensional lake model (FLake, v1)

机译:使用调整后的一维湖泊模型(FLake,v1)确定全世界的湖泊地表水温

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摘要

A tuning method for FLake, a one-dimensional (1-D) freshwater lake model, is applied for the individual tuning of 244 globally distributed large lakes using observed lake surface water temperatures (LSWTs) derived from along-track scanning radiometers (ATSRs). The model, which was tuned using only three lake properties (lake depth, snow and ice albedo and light extinction coefficient), substantially improves the measured mean differences in various features of the LSWT annual cycle, including the LSWTs of saline and high altitude lakes, when compared to the observed LSWTs. Lakes whose lake-mean LSWT persists below 1 °C for part of the annual cycle are considered to be seasonally ice-covered. For trial seasonally ice-covered lakes (21 lakes), the daily mean and standard deviation (2σ) of absolute differences between the modelled and observed LSWTs are reduced from 3.07 °C ± 2.25 °C to 0.84 °C ± 0.51 °C by tuning the model. For all other trial lakes (14 non-ice-covered lakes), the improvement is from 3.55 °C ± 3.20 °C to 0.96 °C ± 0.63 °C. The post tuning results for the 35 trial lakes (21 seasonally ice-covered lakes and 14 non-ice-covered lakes) are highly representative of the post-tuning results of the 244 lakes.ududFor the 21 seasonally ice-covered lakes, the modelled response of the summer LSWTs to changes in snow and ice albedo is found to be statistically related to lake depth and latitude, which together explain 0.50 (R2adj, p = 0.001) of the inter-lake variance in summer LSWTs. Lake depth alone explains 0.35 (p = 0.003) of the variance.ududLake characteristic information (snow and ice albedo and light extinction coefficient) is not available for many lakes. The approach taken to tune the model, bypasses the need to acquire detailed lake characteristic values. Furthermore, the tuned values for lake depth, snow and ice albedo and light extinction coefficient for the 244 lakes provide some guidance on improving FLake LSWT modelling.
机译:一维(1-D)淡水湖模型FLake的调整方法,用于使用从沿轨扫描辐射计(ATSR)得出的观测湖表面水温(LSWT)对244个全球分布的大型湖泊进行单独调整。该模型仅使用三个湖泊属性(湖泊深度,冰雪反照率和消光系数)进行了调整,从而大大改善了LSWT年周期各种特征(包括盐湖和高海拔湖泊的LSWT)的实测平均差异,与观察到的LSWT相比。湖泊平均LSWT在一年周期的一部分内持续低于1 C的湖泊被认为是季节性冰雪覆盖的。对于试验性季节性冰雪覆盖湖泊(21个湖泊),通过调整,模拟和观察到的最小水WT的绝对差的日均值和标准偏差(2σ)从3.07°C±2.25°C降低到0.84°C±0.51°C该模型。对于所有其他试验湖泊(14个非冰雪覆盖的湖泊),改善幅度从3.55°C±3.20°C升至0.96°C±0.63°C。 35个试验湖泊(21个季节性冰雪覆盖的湖泊和14个非冰雪覆盖的湖泊)的调整后结果高度代表了244个湖泊的调整后结果。 ud ud对于21个季节性冰雪覆盖的湖泊,夏季LSWTs对冰雪反照率变化的模型响应被发现与湖的深度和纬度在统计上相关,共同解释了夏季LSWTs的湖间变化的0.50(R2adj,p = 0.001)。单靠湖泊深度可以解释方差的0.35(p = 0.003)。 ud ud许多湖泊没有湖泊特征信息(雪和冰反射率以及消光系数)。调整模型所采用的方法无需获取详细的湖泊特征值。此外,针对244个湖泊的湖泊深度,冰雪反照率和消光系数的调整值为改进FLake LSWT模型提供了一些指导。

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