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Improved mapping and change detection of the start of the crop growing season in the US Corn Belt from long-term AVHRR NDVI

机译:从长期AVHRR NDVI改进了美国玉米带中作物生长季节开始的映射和变更检测

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Long-term monitoring of crop phenology is a critical process to understand changes in cropland vegetation dynamics related to climate and human management. During the last four decades, seasonal changes in vegetation have been measured by satellite instruments, the Advanced Very High Resolution Radiometers (AVHRRs). However, an acceptable detection of crop phenology has been prevented due to its coarse spatial resolution (similar to 8 km) pixels in which croplands are frequently mixed with non-cropland. This study introduces a novel method for detecting the start of the growing season in cropland (SOSC) from the AVHRR Normalized Difference Vegetation Index (NDVI) to examine the long-term changes in SOSC at the 8-km pixel level across the core cropping regions of the Midwestern United States (the so-called 'the Corn Belt') for 1982-2015. The AVHRR-based SOSC was compared with the SOSC retrieved from the pixels covering mostly croplands of the 250-m Moderate Resolution Imaging Spectroradiometer (MODIS) NDVI. These two satellite-based SOSC shows reasonable correspondence in spatial patterns so that the annual values of the root mean square difference ranges from 3.6 to 7.4 days during the overlapping period of 2008-2015. Also, an acceptable correspondence was found between the interannual variations in the AVHRR SOSCs and in the state-level survey of crop stages. For sowing stages, correlation coefficients ranged from 0.43 to 0.68; for flowering stages those ranged from 0.51 to 0.83. By analyzing long-term SOSC changes with climate factors, we found a strong tendency that warmer pre-season condition is accompanied with earlier SOSC. In addition, larger pre-season precipitation tends to postpone SOSC as strongly as the pre-season temperature affects SOSC in a considerable portion of the core cropland. This study suggests that the postponing of sowing due to larger precipitation, which has rarely been highlighted in previous studies, requires more attentions in order for better understanding of vegetation dynamics in agriculture-climate studies.
机译:作物候选的长期监测是了解与气候和人类管理有关的农田植被动态的变化的关键过程。在过去的四十年中,卫星仪器测量了植被的季节变化,先进的非常高分辨率的辐射仪(AVHRRS)。然而,由于其粗糙的空间分辨率(类似于8km)像素,因此已经阻止了作物候选的可接受的检测,其中农田经常与非耕地混合。本研究介绍了一种从AVHRR归一化差异植被指数(NDVI)的农作物(SOSC)中生长季节开始的新方法,以检查核心裁剪区域的8公里像素水平的SOSC中的长期变化1982 - 2015年,美国中西部(所谓的“玉米带”)。将基于AVHRR的SOSC与从覆盖250-M适度分辨率成像分光辐射器(MODIS)NDVI的大多数农作物的像素中检索的SOSC进行了比较。这两种基于卫星的SOSC显示了空间模式的合理对应,使得根部均值的年值范围为2008 - 2015年重叠期间的3.6至7.4天。此外,在AVHRR SOSC的续际变化和作物阶段的状态级调查之间发现了可接受的对应关系。对于播种阶段,相关系数范围为0.43至0.68;对于开花阶段,那些范围为0.51至0.83。通过分析气候因素的长期SOSC变化,我们发现了温暖的季节条件伴随着早期的SOSC的强烈趋势。此外,随着季节性温度影响SOSC,较大的季季沉淀趋于推迟SOSC,在核心农田的相当大部分中影响SOSC。本研究表明,由于较大的降水,在以前的研究中突出的沉淀导致播种,需要更多的注意力,以便更好地了解农业 - 气候研究中的植被动态。

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