Open AccessAsymmetric seasonal daytime and nighttime warming and its effects on vegetation in the Loess Plateau
Author(s) -
Liqun Ma,
Fen Qin,
Hao Wang,
Yaochen Qin,
Haoming Xia
Publication year - 2019
Publication title -
plos one
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.99
H-Index - 332
ISSN - 1932-6203
DOI - 10.1371/journal.pone.0218480
Subject(s) - daytime , environmental science , normalized difference vegetation index , plateau (mathematics) , loess plateau , atmospheric sciences , grassland , vegetation (pathology) , precipitation , global warming , loess , climatology , seasonality , climate change , physical geography , ecology , biology , geography , geology , soil science , meteorology , medicine , mathematical analysis , paleontology , mathematics , pathology
Over the period 1982–2015, temperatures have exhibited an asymmetric warming pattern diurnally, as well as seasonally across the Loess Plateau. However, very limited research has studied the implications and effects of such seasonally heterogeneous warming across the Loess Plateau. In this study, we also analyzed the time series trends and seasonal spatial patterns of the maximum ( T max ) and minimum ( T min ) temperatures and evaluated how different vegetation responded to daytime and nighttime warming in the Loess Plateau from 1982 to 2015 based on the NDVI and meteorological parameters (precipitation or temperature). We found that T max and T min significantly increased throughout the years except for T max in autumn, and the diurnal asymmetric warming showed some striking seasonal differences. For example, the increasing rates of T min in spring, summer, autumn, and winter were 0.75, 1.20, 1.88, and 1.10 times larger than that of T max , respectively. NDVI showed significantly positive correlation with T max and T min in spring and winter, while NDVI presented significantly positive correlation with T min in summer and T max in autumn across entire Loess Plateau. Furthermore, we also discovered diverse seasonal responses in terms of vegetation types to daytime and nighttime warming. For instance, Spring NDVI showed significantly positive partial correlations with T max and T min . In summer, grasslands and wetlands merely displayed significantly positive partial correlations with T min . Cultivated land presented significantly positive partial correlation between the NDVI and T max ( T min ) in autumn. In winter, cultivated land, forest, and grassland exhibited significantly positive partial correlation with T max and T min , while only wetland showed a significantly positive partial correlation with T max . Our results demonstrated responses of vegetation to climate extremes and enhance a better understanding of the seasonally different responses of vegetation under global climate change at different scale.