Multi-Climate Factors and the Preceding Growth Stage of Vegetation Co-Regulated the Variation of the End of Growing Season in Northeast Inner Mongolia, China

Abstract

The end of growing season (EOS) is an effective indicator of annual vegetation growth. Previous studies have revealed the dynamics of the EOS with climate change, while the influence of vegetation growth in preceding stage and peak of growing season (POS) on the EOS has not been thoroughly documented. In this study, we used four smoothing methods to obtain EOS dates from the Normalized Difference Vegetation Index (NDVI) in northeast Inner Mongolia (NIM) between 2001-2017, assessed the differences in the spatiotemporal variations of the EOS obtained by the four smoothing methods, and then investigated the impacts of climate factors, summer/ autumn vegetation growth and POS on the EOS. The results showed that the EOS dates obtained with different smoothing methods were broadly consistent in terms of their spatial patterns and temporal trends. In terms of climate factors, the EOS was driven mainly by preseason precipitation for the majority of vegetation types and advanced with increasing precipitation. For the steppe, both minimum temperature (Tmin) and relative humidity (RHU) played the most important roles in regulating the variation of EOS which was delayed with an increase in Tmin and reduction in RHU. Furthermore, our study found an earlier POS and vigorous vegetation growth in summer would jointly advance the steppe EOS, but these relationships were the opposite of each other in meadow and forest regions. Interestingly, the EOS of NIM was more related with vegetation growth in the most recent period before the EOS. This study highlights the importance of ecological processes in the preceding growth stage for understanding the dynamics of EOS. INDEX TERMSEnd of growing season, Northeast Inner Mongolia, Climate change, Peak of growing season, Preceding growth stage of vegetation This work is licensed under a Creative Commons Attribution 4.

Variation in Vegetation Phenology and Its Response to Climate Change in Marshes of Inner Mongolian

“…This implied that the increases of T min and T max in August delayed the marshes EOS in Inner Mongolia, but increasing T min had a stronger delaying effect on the EOS than that in T max . The delaying effect of warming T max on EOS may be due to the fact that the increase in T max can improve the activities of photosynthetic enzymes and promote photosynthesis [51]. By contrast, although the increase of T min can cause more organic matter consumption, increasing T min can also cause a compensation effect for marsh vegetation [52].…”

Console-Based Mapping of Mongolia Using GMT Cartographic Scripting Toolset for Processing TerraClimate Data

“…Actual and regular updates of mapping help to increase the control on possible drought distribution and climate characteristics, such as temperature, vapour, snow water equivalent, and the like. The study aimed to the development and maintaining of agricultural monitoring system in Mongolia or Inner Mongolia (China), following the existing studies [115][116][117]. In such a way, the extended study can reach the goal to increase environmental monitoring of Mongolia using maps made by GMT.…”