Published July 2013 | Version v1
Journal article

Vegetation response to extreme climate events on the Mongolian Plateau from 2000 to 2010

  • 1. Department of Environmental Sciences, University of Toledo, Toledo, OH 43606 (United States)
  • 2. Earth Systems Research Center, Institute for the Study of Earth, Oceans, and Space,University of New Hampshire, Durham, NH (United States)
  • 3. Atmospheric and Environmental Research Incorporated, Boston, MA (United States)
  • 4. Bay Area Environmental Research Institute and NASA Ames Research Center, Moffett Field,CA 94035 (United States)
  • 5. College of Global Change and Earth System Science, Beijing Normal University, Beijing 100875 (China)
  • 6. Institute of Geography, Mongolian Academy of Sciences, Ulaanbaatar, 210620 (Mongolia)

Description

Climate change has led to more frequent extreme winters (aka, dzud) and summer droughts on the Mongolian Plateau during the last decade. Among these events, the 2000–2002 combined summer drought–dzud and 2010 dzud were the most severe on vegetation. We examined the vegetation response to these extremes through the past decade across the Mongolian Plateau as compared to decadal means. We first assessed the severity and extent of drought using the Tropical Rainfall Measuring Mission (TRMM) precipitation data and the Palmer drought severity index (PDSI). We then examined the effects of drought by mapping anomalies in vegetation indices (EVI, EVI2) and land surface temperature derived from MODIS and AVHRR for the period of 2000–2010. We found that the standardized anomalies of vegetation indices exhibited positively skewed frequency distributions in dry years, which were more common for the desert biome than for grasslands. For the desert biome, the dry years (2000–2001, 2005 and 2009) were characterized by negative anomalies with peak values between −1.5 and −0.5 and were statistically different (P < 0.001) from relatively wet years (2003, 2004 and 2007). Conversely, the frequency distributions of the dry years were not statistically different (p < 0.001) from those of the relatively wet years for the grassland biome, showing that they were less responsive to drought and more resilient than the desert biome. We found that the desert biome is more vulnerable to drought than the grassland biome. Spatially averaged EVI was strongly correlated with the proportion of land area affected by drought (PDSI <− 1) in Inner Mongolia (IM) and Outer Mongolia (OM), showing that droughts substantially reduced vegetation activity. The correlation was stronger for the desert biome (R2 = 65 and 60, p < 0.05) than for the IM grassland biome (R2 = 53, p < 0.05). Our results showed significant differences in the responses to extreme climatic events (summer drought and dzud) between the desert and grassland biomes on the Plateau. (letter)

Availability note (English)

Available from http://dx.doi.org/10.1088/1748-9326/8/3/035033

Additional details

Identifiers

Publishing Information

Journal Title
Environmental Research Letters
Journal Volume
8
Journal Issue
3
Journal Page Range
[12 p.]
ISSN
1748-9326

INIS

Country of Publication
United Kingdom
Country of Input or Organization
International Atomic Energy Agency (IAEA)
INIS RN
44083813
Subject category
S54: ENVIRONMENTAL SCIENCES;
Descriptors DEI
ATMOSPHERIC PRECIPITATIONS; CHINA; CLIMATES; CLIMATIC CHANGE; DESERTS; DROUGHTS; MONGOLIAN PEOPLES REPUBLIC; RANGELANDS
Descriptors DEC
ARID LANDS; ASIA; ECOSYSTEMS; TERRESTRIAL ECOSYSTEMS