Universities Space Research Association, NASA Marshall Space Flight Center, Huntsville, AL, United States of America.
New York State Department of Health & University at Albany- State University of New York, Albany, NY, United States of America.
PLoS One. 2020 Jan 16;15(1):e0227480. doi: 10.1371/journal.pone.0227480. eCollection 2020.
We have developed and applied a relatively simple disaggregation scheme that uses spatial patterns of Land Surface Temperature (LST) from MODIS warm-season composites to improve the spatial characterization of daily maximum and minimum air temperatures. This down-scaling model produces qualitatively reasonable 1 km daily maximum and minimum air temperature estimates that reflect urban and coastal features. In a 5-city validation, the model was shown to provide improved daily maximum air temperature estimates in the three coastal cities, compared to 12 km NLDAS-2 (North American Land Data Assimilation System). Down-scaled maximum temperature estimates for the other two (non-coastal) cities were marginally worse than the original NLDAS-2 temperatures. For daily minimum temperatures, the scheme produces spatial fields that qualitatively capture geographic features, but quantitative validation shows the down-scaling model performance to be very similar to the original NLDAS-2 minimum temperatures. Thus, we limit the discussion in this paper to daily maximum temperatures. Overall, errors in the down-scaled maximum air temperatures are comparable to errors in down-scaled LST obtained in previous studies. The advantage of this approach is that it produces estimates of daily maximum air temperatures, which is more relevant than LST in applications such as public health. The resulting 1 km daily maximum air temperatures have great potential utility for applications such as public health, energy demand, and surface energy balance analyses. The method may not perform as well in conditions of strong temperature advection. Application of the model also may be problematic in areas having extreme changes in elevation.
我们开发并应用了一种相对简单的分解方案,该方案利用 MODIS 暖季合成数据中的地表温度(LST)空间模式来改善日最高和最低气温的空间特征。该降尺度模型生成了定性合理的 1km 日最高和最低气温估计值,反映了城市和沿海特征。在 5 个城市的验证中,与 12km 的 NLDAS-2(北美陆面数据同化系统)相比,该模型在三个沿海城市提供了改进的日最高气温估计值。对于另外两个(非沿海)城市,降尺度最大温度估计值略逊于原始 NLDAS-2 温度。对于日最低温度,该方案生成的空间场定性地捕捉了地理特征,但定量验证表明降尺度模型性能与原始 NLDAS-2 最低温度非常相似。因此,我们在本文的讨论中仅限于日最高温度。总体而言,降尺度最大空气温度的误差与先前研究中获得的降尺度 LST 的误差相当。该方法的优势在于它生成了日最高气温的估计值,这在公共卫生等应用中比 LST 更相关。生成的 1km 日最高空气温度对于公共卫生、能源需求和表面能量平衡分析等应用具有很大的潜在用途。在温度平流较强的情况下,该模型的性能可能不如预期。在海拔变化剧烈的地区,模型的应用也可能存在问题。