Abstract

Climate change caused by land use/cover change (LUCC) is becoming a hot topic in current global change, especially the changes caused by the grassland degradation. In this paper, based on the baseline underlying surface data of 1993, the predicted underlying surface data which can be derived through overlaying the grassland degradation information to the map of baseline underlying surface, and the atmospheric forcing data of RCP 6.0 from CMIP5, climatological changes caused by future grassland changes for the years 2010–2020 and 2040–2050 with the Weather Research Forecast model (WRF) are simulated. The model-based analysis shows that future grassland degradation will significantly result in regional climate change. The grassland degradation in future could lead to an increasing trend of temperature in most areas and corresponding change range of the annual average temperature of −0.1°C–0.4°C, and it will cause a decreasing trend of precipitation and corresponding change range of the annual average precipitation of 10 mm–50 mm. This study identifies lines of evidence for effects of future grassland degradation on regional climate in Mongolia which provides meaningful decision-making information for the development and strategy plan making in Mongolia.

Highlights

  • During the last millennium, human beings have changed natural ecosystems, such as converting forest lands and grasslands into croplands, pastures, and bare soil [1]

  • Global mean surface air temperature increased with a rate of 0.07∘C per decade from 1906 to 2005 [7]. It seems that the magnitude of importance of land use and cover changes (LUCC) on future climate can only be determined by knowing and understanding how certain land conversions directly impact on climate on regional scales

  • The effects of future grassland degradation on climate were measured by the difference of the simulated results with baseline and predicted underlying surfaces, which can reduce the simulated bias induced by discontinuous simulation

Read more

Summary

Introduction

Human beings have changed natural ecosystems, such as converting forest lands and grasslands into croplands, pastures, and bare soil [1]. Global mean surface air temperature increased with a rate of 0.07∘C per decade from 1906 to 2005 [7] It seems that the magnitude of importance of LUCC on future climate can only be determined by knowing and understanding how certain land conversions directly impact on climate on regional scales. Previous studies showed that increase of grassland since preindustrial times has caused an overall warming trend in both mean and extreme temperatures which is detectable in the observed temperature changes [27, 28] The warming in both mean and extreme temperatures due to anthropogenic forcing other than land use is detected in all cases, whereas the relatively weak effect of natural climatic forcing is not detected in any research.

Case Study Area
Data and Methodology
Results
Conclusion and Discussion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call