B1 B Bolortsetseg AS06

Past and present climate change impacts on rangeland production: 

Past and present climate change impacts on rangeland production Bolortsetseg B., Erdenetuya M., Sanjid S., Manibazar N., Gantsetseg B., Bat-Oyun Ts.

Impact of climate change: 

Impact of climate change Introduction to rangeland Rangeland productivity Pasture carrying capacity Plant phenology Plant population Land cover change Modeling of rangeland ecosystem

Introduction to rangeland: 

Introduction to rangeland The total agricultural used land - 130541.3 thousand ha in Mongolia Pasture – 97.5 % (127307.0 thousand ha) Hay – 1.5 % (1986.6 thousand ha) Agricultural land per person - 53.8 ha (20 times the world average) Livestock –23.6 million Scientific research of vegetation has started since 1950 by Russian scientists and national specialists. Geobotanical field surveys were done in 1950-1955, water resource exploration expedition in 1959-1961, rangeland mapping and expedition in 1991-1992.

Rangeland ecosystems: 

Rangeland ecosystems The high mountain belt The mountain taiga belt The forest steppe The steppe The desert steppe The desert

Rangeland biomass: 

Rangeland biomass Data: Rangeland monitoring biomass data of 64 sites for 1966-2001 Changes in biomass, g/m2/1year Biomass, 100kg/ha

Rangeland biomass (continued): 

Rangeland biomass (continued) Peak biomass trend at Arvaiheer (steppe), Erdenemandal (forest steppe), Mandalgobi (desert steppe), Ulgii (Altai mountains)

Pasture carrying capacity: 

Pasture carrying capacity The total pasture carrying capacity - 44.5 million sheep unit based on average observed peak biomass. Based on the decreasing trend of peak biomass by 20-30 %, the total pasture capacity was calculated as 32.6 million sheep unit. Past 40 years the total pasture carrying capacity was drop down by 27 % because of biomass decrease.

Pasture carrying capacity: 

Pasture carrying capacity The total pasture carrying capacity - 44.5 million sheep unit based on average observed peak biomass. Based on the decreasing trend of peak biomass by 20-30 %, the total pasture capacity was calculated as 32.6 million sheep unit. Past 40 years the total pasture carrying capacity was drop down by 27 % because of biomass decrease.

Plant phenology: 

Plant phenology Phenological date of 8 dominant plants such as Agropyron sp., Cleistogenes sp., Festuca sp., Leymus chinensis, Stipa sp., Carex sp., Allium polyrrhizum and Artemisia frigida was analysed and defined their trends. Time series longer than 15 years were selected for the analysis. Plants emergency is tend to start earlier in the forest steppe and the steppe. In the Altai mountains, the desert steppe and the desert some of plants (Artemisia frigida, Stipa sp.) have had delayed onset trend. Plant senescence occurred earlier in the forest steppe, the steppe and the Altai mountains, later in the desert steppe and the desert.  

Plant phenology (continued): 

Plant phenology (continued) Because of extended drought, some plants such as Allium polirrhizum, Rheum nanum, Limonium tenellum, Ferula bungeana and etc. have not flowered and develop just after rain. As a result, summer flowering plants have been become to flower early spring or late autumn and flowering occurred indefinite time. Some plants such as Pulsatilla, Caragana sp. have flowered in autumn which is considered as plant special responces to environmental negative effects. Flowering rhythm changes in the desert steppe  

Plant population: 

Plant population Plant composition and species number changes of communities with Leymus - Potentilla bifurca, Leymus chinensis – Stipa krylovii, Agrostis mongolica – Carex orthostachys, Carex orthostacys – Potentilla anserine in Orkhon meadow. Due to field survey of communities with Leymus - Potentilla bifurca, Leymus chinensis – Stipa krylovii, Agrostis mongolica – Carex orthostachys, Carex orthostacys – Potentilla anserine, plant composition and species numbers in autumn of 2002 are more than in the beginning of 1980 years that those years were very dry, but less than in the middle of 1980 years. In some sources, biomass of low nutrient plants increased and production of high quality plants decreased because of intensified grazing. Source: Manibazar N

Land cover change: 

Land cover change 1992 1997 2002

Modeling of rangeland ecosystem: 

Modeling of rangeland ecosystem Century 4.0 is used for the study. 37 sites in different ecosystems were selected. 0.5x0.5 0 grids were prepared. Monthly climate data were input. Soil data () for sites and grids were defined in the model. Plant composition C3:C4 was defined The average annual nitrogen (N) fixation rate was defined as 0.2 to 0.8 g/m-2 year-1.

Modeling of soil organic matter: 

Modeling of soil organic matter Soil organic C Soil organic N Comparison of simulated and actual steady state soil carbon and nitrogen

Soil organic matter changes for past 40 years: 

Soil organic matter changes for past 40 years Soil organic N Soil organic C According to soil organic matter changes distribution, soil organic matter raised in the north part of the forest steppe and the eastern steppe. Generally in the southern part of the country had decreased trend of soil organic matter.

Simulation of rangeland biomass: 

Simulation of rangeland biomass Comparison of simulated and actual biomass Simulated aboveground live peak biomass, g/m2

Rangeland peak biomass changes: 

Rangeland peak biomass changes Annual NPP, biomass and biomass and rainfall changes for 1961-2000 years

Rangeland spring biomass and its changes: 

Rangeland spring biomass and its changes Spring biomass and biomass and precipitation changes

Thank you for your attention: 

Thank you for your attention