Abstract

Urbanization and the resulting increase in development areas and populations cause micro-climate changes such as the urban heat island (UHI) effect. This micro-climate change can affect vegetation phenology. It can advance leaf unfolding and flowering and delay the timing of fallen leaves. This study was carried out to clarify the impact of urbanization on the leaf unfolding of Mongolian oak. The survey sites for this study were established in the urban center (Mts. Nam, Mido, and Umyeon in Seoul), suburbs (Mts. Cheonggye and Buram in Seoul), a rural area (Gwangneung, Mt. Sori in Gyeonggi-do), and a natural area (Mt. Jeombong in Gangwon-do). Green-up dates derived from the analyses of digital camera images and MODIS satellite images were the earliest in the urban center and delayed through the suburbs and rural area to the natural area. The difference in the observed green-up date compared to the expected one, which was determined by regarding the Mt. Jeombong site located in the natural area as the reference site, was the biggest in the urban center and decreased through the suburbs and rural area to the natural area. Green-up dates in the rural area, suburbs, and urban center were earlier by 11.0, 14.5, and 16.3 days than the expected ones. If these results are transformed into the air temperature based on previous research results, it could be deduced that the air temperature in the urban center, suburbs, and rural area rose by 3.8 to 4.6 °C, 3.3 to 4.1 °C, and 2.5 to 3.1 °C, respectively. Green-up dates derived based on the accumulated growing degree days (AGDD) showed the same trend as those derived from the image interpretation. Green-up dates derived from the change in sap flow as a physiological response of the plant showed a difference within one day from the green-up dates derived from digital camera and MODIS satellite image analyses. The change trajectory of the curvature K value derived from the sap flow also showed a very similar trend to that of the curvature K value derived from the vegetation phenology. From these results, we confirm the availability of AGDD and sap flow as tools predicting changes in ecosystems due to climate change including phenology. Meanwhile, the green-up dates in survey sites were advanced in proportion to the land use intensity of each survey site. Green-up dates derived based on AGDD were also negatively correlated with the land use intensity of the survey site. This result implies that differences in green-up dates among the survey sites and between the expected and observed green-up dates in the urban center, suburbs, and rural area were due to the increased temperature due to land use in the survey sites. Based on these results, we propose conservation and restoration of nature as measures to reduce the impact of climate change.

Highlights

  • Urbanization is one of the major social and scientific changes spreading around the world [1,2]

  • A natural forest, there is an artificial influence, indicating a difference in the green-up date (Table 4). By comparing these results by landscape type according to land use intensity, this showed the biggest difference in the urban center as the difference between the observed date and the expected date of each study site was 11 days in the rural area, about 14.5 days in the suburbs, and about 16.3 days in the urban center (Table 4)

  • The relationship between the phenology response of Mongolian oak and land use intensity was investigated by determining the green-up date of plants through digital camera image and MODIS satellite image analyses

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Summary

Introduction

Urbanization is one of the major social and scientific changes spreading around the world [1,2]. It significantly alters land surface conditions and has profound impacts on terrestrial ecosystem processes and services [3,4,5,6,7]. An increase in atmospheric CO2 due to intensive use of land and fossil fuel destroys the balance of the global carbon cycle maintained in an equilibrium fashion [2,8,9,10,11]. Inadvertent weather factor changes in urban areas form an important effect on regional climate change [13,14,15,16] Increased development areas and populations cause changes in weather factors and affect terrestrial ecosystems [3,4,5,6,12].

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