Variability and change of climate extremes from indigenous herder knowledge and at meteorological stations across central Mongolia

Abstract

In semi-arid regions, air temperatures have increased in the last decades more than in many other parts of the world. Mongolia has an arid/semi-arid climate and much of the population are herders whose livelihoods depend upon limited water resources that fluctuate with a variable climate. Herders were surveyed to identify their observations of changes in climate extremes for two soums of central Mongolia, Ikh-Tamir in the forest steppe north of the Khangai Mountains and Jinst in the desert steppe south of the mountains. The herders’ indigenous knowledge of changes in climate extremes mostly aligned with the station-based analyses of change. Temperatures were warming with more warm days and nights at all stations. There were fewer cool days and nights observed at the mountain stations both in the summer and winter, yet more cool days and nights were observed in the winter at the desert steppe station. The number of summer days is increasing while the number of frost days is decreasing at all stations. The results of this study support further use of local knowledge and meteorological observations to provide more holistic analysis of climate change in different regions of the world.

Keywords

climate change / climate extreme indices / indigenous knowledge systems / temperature / precipitation

References

[1] Alexander C, Bynum N, Johnson E, King U, Mustonen T, Neofotis P, Oettlé N, Rosenzweig C, Sakakibara C, Shadrin V, Vicarelli M, Waterhouse J, Weeks B (2011). Linking indigenous and scientific knowledge of climate change. Bioscience, 61(6): 477–484

[2] Angerer J, Han G, Fujisaki I, Havstad K (2008). Rangelands, 30(3): 46–51

[3] Auerbach C F, Silverstein L B (2003). Qualitative Data: an Introduction to Coding and Analysis. New York: New York University Press

[4] Ayanlade A, Radeny M, Morton J F (2017). Comparing smallholder farmers’ perception of climate change with meteorological data: a case study from southwestern Nigeria. Weather Clim Extrem, 15: 24–33

[5] Baival B, Oyuntulkhuur B, Altanzul T, Fernández-Giménez M E (2011). A case study of community-based rangeland management in Jinst Soum, Mongolia. In: Fernández-Giménez M E, Wang X, Baival B, Klein J, Reid R, eds. Restoring Community Connections to the Land: Building Resilience through Community-based Rangeland Management in China and Mongolia. Wallingford: CABI Press

[6] Barnhardt R, Oscar Kawagley A (2005). Indigenous knowledge systems and Alaska Native ways of knowing. Anthropol Educ Q, 36(1): 8–23

[7] Batima P (2006). Climate Change Vulnerability and Adaptation in the Livestock Sector of Mongolia: A Final Report Submitted to Assessments of Impacts and Adaptations to Climate Change (AIACC), International START Secretariat: Project No. AS 06

[8] Batima P, Dagvadorj D (2000). Climate Change and Its Impacts in Mongolia. Mongolia: JEMR Publishing

[9] Beniston M, Stephenson D B (2004). Extreme climate events and their evolution under changing climatic conditions. Global Planet Change, 44(1-4): 1–9

[10] Bohensky E L, Maru Y (2011). Indigenous knowledge, science, and resilience: what have we learned from a decade of international literature on integration? Ecol Soc, 16(4): 6

[11] Brooke L F (2017). The participation of indigenous peoples and the application of their environmental and ecological knowledge in the Arctic Environmental Protection Strategy. In: Proceedings of the Inuit Circumpolar Conference. Ottawa, 28–30

[12] Bruegger R A, Jigjsuren O, Fernández-Giménez M E (2014). Herder observations of rangeland change in Mongolia: indicators, causes, and application to community-based management. Rangeland Ecol Manag, 67(2): 119–131

[13] Dagvadorj D, Natsagdorj L, Dorjpurev J, Namkhainyam B (2009). Mongolia: Assessment Report on Climate Change. Ministry of Nature, Environment and Tourism, Mongolia

[14] Davi N K, Jacoby G C, D’Arrigo R D, Baatarbileg N, Jinbao L, Curtis A E (2009). A tree-ring based drought index reconstruction for far-western Mongolia. Int J Climatol, 29(10): 1508–1514

[15] Dorligsuren D, Batbuyan B, Bulgamaa D, Fassnacht S R (2011). Lessons from a territory-based community development approach in Mongolia: Ikh-tamir Pasture user groups. In: Fernández-Giménez M E, Wang X, Baival B, Klein J, Reid R, eds. Restoring Community Connections to the Land: Building Resilience through Community-based Rangeland Management in China and Mongolia. Oxfordshire: CABI Press

[16] Fassnacht S R, Sukh T, Fernández-Giménez M E, Batbuyan B, Venable N B H, Laituri M, Adyabadam G (2011). Local understanding of hydro-climatic changes in Mongolia. In: IAHS Proceedings of symposium Cold Region Hydrology in a Changing Climate held during IUGG2011. Melbourne: 120–129

[17] Fassnacht S R, Venable N B H, Khishigbayar J, Cherry M L (2013). The probability of precipitation as snow derived from daily air temperature for high elevation areas of Colorado, United States. In: IAHS-IAPSO-IASPEI Proceedings of symposium Assembly Cold and Mountain Region Hydrological Systems Under Climate Change: Towards Improved Projections, Gothenburg: 65–70

[18] Fassnacht S R, Cherry M L, Venable N B H, Saavedra F (2016). Snow and albedo climate change impacts across the United States Northern Great Plains. Cryosphere, 10(1): 329–339

[19] Fassnacht S R, López-Moreno J I, Ma C, Weber A N, Pfohl A K D, Kampf S K, Kappas M (2017). Spatio-temporal snowmelt variability across the headwaters of the southern Rocky Mountains. Front Earth Sci, 11(3): 505–514

[20] Fassnacht S R, Allegretti A M, Venable N B H, Fernández-Giménez M E, Tumenjargal S, Kappas M, Laituri M J, Batbuyan B, Pfohl A K D (2018a). Merging indigenous knowledge systems and station observations to estimate uncertainty of precipitation change in central mongolia. Hydrology, 5(3): 46

[21] Fassnacht S R, Venable N B H, McGrath D, Patterson G G (2018b). Sub-seasonal snowpack trends in the Rocky Mountain National Park area, Colorado USA. Water, 10(5): 562

[22] Fernandez-Gimenez M E (2000). The role of Mongolian nomadic pastoralists’ ecological knowledge in rangeland management. Ecol Appl, 10: 1318–1326

[23] Fernández-Giménez M E, Batkhishig B, Batbuyan B (2012). Cross-boundary and cross-level dynamics increase vulnerability to severe winter disasters (dzud) in Mongolia. Glob Environ Change, 22(4): 836–851

[24] Fernández-Giménez M E, Angerer J P, Allegretti A, Fassnacht S R, Byamba A, Chantsallkham J, Reid R, Venable N B H (2015a). Integrating herder observations, meteorological data and remote sensing to understand climate change patterns and impacts across an eco-climatic gradient in Mongolia. In: Fernández-Giménez M E, Batkhishig B, Fassnacht S R, Wilson D, eds. Proceedings of Building Resilience of Mongolian Rangelands: A Trans-disciplinary Research Conference, Ulaanbaatar, 228–234

[25] Fernández-Giménez M E, Batkhishig B, Batbuyan B, Ulambayar T (2015b). Lessons from the dzud: community-based rangeland management increases adaptive capacity of Mongolian herders to winter disasters. World Dev, 68: 48–65

[26] Fernández-Giménez M E, Venable N H, Angerer J, Fassnacht S R, Reid R S, Khishigbayar J (2017). Exploring linked ecological and cultural tipping points in Mongolia. Anthropocene, 17: 46–69

[27] Flanagan C, Laituri M (2004). Local cultural knowledge and water resource management: the Wind River Indian Reservation. Environ Manage, 33(2): 262–270

[28] Folland C K, Miller C, Bader D, Crowe M, Jones P, Plummer N, Richman M, Parker D E, Rogers J, Scholefield P (1999). Workshop on indices and indicators for climate extremes, Asheville, NC, USA, 3–6 June 1997 Breakout Group C: Temperature Indices for Climate Extremes. Clim Change, 42(1): 31–43

[29] Fosu-Mensah B Y, Vlek P L, MacCarthy D (2012). Farmers’ perception and adaptation to climate change: a case study of Sekyedumase district in Ghana. Environ Dev Sustain, 14(4): 495–505

[30] Gearheard S, Pocernich M, Stewart R, Sanguya J, Huntington H (2010). Linking Inuit knowledge and meteorological station observations to understand changing wind patterns at Clyde River, Nunavut. Clim Change, 100(2): 267–294

[31] Gilbert R O (1987). Statistical Methods for Environmental Pollution Monitoring. New York: John Wiley & Sons

[32] Gong D, Wang S (2000). Severe summer rainfall in China associated with enhanced global warming. Clim Res, 16: 51–59

[33] Goulden C E, Mead J, Horwitz R, Goulden M, Nandintsetseg B, McCormick S, Boldgiv B, Petraitis P S (2016). Interviews of Mongolian herders and high resolution precipitation data reveal an increase in short heavy rains and thunderstorm activity in semi-arid Mongolia. Clim Change, 136(2): 281–295

[34] Groisman P, Karl T, Easterling D, Knight R, Jamason P, Hennessy K, Suppiah R, Page C, Wibig J, Fortuniak K, Razuvaev V, Douglas A, Forland E, Zhai P (1999). Changes in the probability of extreme precipitation: important indicators of climate change. Clim Change, 42(1): 243–283

[35] Hou X Y, Han Y, Li F Y (2012). The perception and adaptation of herdsmen to climate change and climate variability in the desert steppe region of northern China. Rangeland J, 34(4): 349–357

[36] Huntington H (2000). Using traditional ecological knowledge in science methods and applications. Ecol Appl, 10(5): 1270–1274

[37] Huntington H, Callaghan T, Fox S, Krupnik I (2004). Matching traditional and scientific observations to detect environmental change: a discussion on Arctic terrestrial ecosystems. Ambio, 13(Spec No): 18–23

[38] Inglis J T (1993). Traditional Ecological Knowledge: Concepts and Cases. Ottawa: Canadian Museum of Nature

[39] Iwasaki H, Nii T (2006). The break in the mongolian rainy season and its relation to the stationary rossby wave along the Asian Jet. J Clim, 19(14): 3394–3405

[40] Jiri O, Mafongoya P L, Chivenge P (2015). Indigenous knowledge systems, seasonal ‘quality’ and climate change adaptation in Zimbabwe. Clim Res, 66(2): 103–111

[41] Karl T R, Knight R W, Easterling D R, Quayle R G (1996). Indices of climate change for the United States. Bull Am Meteorol Soc, 77(2): 279–292

[42] Kendall M G, Gibbons J D (1990). Rank Correlation Methods. 5th ed. London: Edward Arnold, a Division of Hodder and Stoughton

[43] Likert R A (1932). Technique for the measurement of attitudes. Arch Psychol, 140: 1–55

[44] Ma C, Fassnacht S R, Kampf S K (2019). How temperature sensor change affects warming trends and modeling—an evaluation across the State of Colorado. Water Resour Res, 55(11): 9748–9764

[45] Ma X, Yasunari T, Ohata T, Natsagdorj L, Davaa G, Oyunbaatar D (2003). Hydrological regime analysis of the Selenge River Basin in Mongolia. Hydrol Processes, 17(14): 2929–2945

[46] Mann H B (1945). Nonparametric tests against trend. Econometrica, 13(3): 245–259

[47] Marin A (2010). Rider under storms: contributions of nomadic herders observations to analyzing climate change in Mongolia. Glob Environ Change, 20(1): 162–176

[48] Nagashima K, Tada R, Toyoda S (2013). Westerly jet-east Asian summer monsoon connection during the Holocene. Geochem Geophys Geosyst, 14(12): 5041–5053

[49] Nakashima D, Roué M (2002). Indigenous knowledge, peoples and sustainable practice. In: Timmerman P, ed. Encyclopedia of Global Environmental Change: Social and economic dimensions of global environmental change, 5: 314–324

[50] NAMHEM (2008). Manual for issuing hazardous weather, hydrologic, and natural phenomena (in Mongolian). 4th ed, National Agency of Meteorology, Hydrology, and Environment Monitoring, Ulaanbaatar

[51] Nandintsetseg B, Greene J S, Goulden C E (2007). Trends in extreme daily precipitation and temperature near Lake Hovsgol, Mongolia. Int J Climatol, 27(3): 341–347

[52] National Statistics Office of Mongolia (2019). Data from the Mongolian Statistical Information Service Tables

[53] Nicholls N, Gruza G V, Jouzel J, Karl T R, Ogallo L A, Parker D E (1996). Observed climate variability and change. In: Houghton J T, Meira Filho L G, Callander B A, Harris N, Kattenberg A, Maskell K eds. Climate Change 1995. The Science of Climate Change: Contribution of Working Group I to the Second Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge: Cambridge University Press, 133–192

[54] Nicholls N, Murray B (1999). Workshop on indices and indicators for climate extremes: Asheville, NC, USA, 3–6 June 1997. Breakout Group B: Precipitation. Clim Change, 42(1): 23–29

[55] Nichols T, Berkes F, Jolly D, Snow N B, Sachs Harbour (N.W.T.) T C (2004). Climate change and sea ice: local observations from the Canadian Western Arctic. Arctic, 57(1): 68–79

[56] Peart N (1977). Xanadu. Track 2 on A Farewell to Kings, Anthem, Toronto Ontario Canada

[57] Peterson T C, Folland C, Gruza G, Hogg W, Mokssit A, Plummer N (2001). Report on the Activities of the Working Group on Climate Change Detection and Related Rapporteurs 1998–2001. Southampton: ICPO Publication

[58] Pielke R A Sr, Stohlgren T, Schell L, Parton W, Doesken N, Redmond K, Moeny J, McKee T, Kittel T G F (2002). Problems in evaluating regional and local trends in temperature: an example from eastern Colorado, USA. Int J Climatol, 22(4): 421–434

[59] Sen P K (1968). Estimates of the regression coefficient based on Kendall’s tau. J Am Stat Assoc, 63(324): 1379–1389

[60] Simelton E, Quinn C H, Batisani N, Dougill A J, Dyer J C, Fraser E D G, Mkwambisi D, Sallu S, Stringer L C (2013). Is rainfall really changing? Farmers’ perceptions, meteorological data, and policy implications. Clim Dev, 5(2): 123–138

[61] Speranza Ch, Kiteme B, Ambenje P, Wiesmann U, Makali S (2010). Indigenous knowledge related to climate variability and change: insights from droughts in semi-arid areas of former Makueni District, Kenya. Clim Change, 100(2): 295–315

[62] Sternberg T (2008). Environmental challenges in Mongolia’s dryland pastoral landscape. J Arid Environ, 72(7): 1294–1304

[63] Sukh T (2012). Local understanding of hydro-climate changes in Mongolia. Dissertation for Master’s Degree, Fort Collins: Colorado State University

[64] Theil H (1950). A rank-invariant method of linear and polynomial regression analysis, I, II, III. Proc R Neth Acad Sci, 53: 386–392, 521–525, 1397–1412

[65] Venable N B H, Fassnacht S R, Adyabadam G, Tumenjargal S, Fernández-Giménez M E, Batbuyan B (2012). Does the length of station record influence the warming trend that is perceived by Mongolian herders near the Khangai Mountains? Pirineos, 167(0): 69–88

[66] Venable N B H, Fassnacht S R, Hendricks A D (2015). Spatial changes in climate across Mongolia. In: Fernández-Giménez M E, Batkhishig B, Fassnacht S R, Wilson D, eds. Proceedings of Building Resilience of Mongolian Rangelands: A Trans-disciplinary Research Conference. Ulaanbaatar: 2015, 73–79

[67] Venable N B H (2016). Trends and tree-rings: an investigation of the historical and paleo proxy hydroclimate record of the Khangai Mountain region of Mongolia. Dissertation for the Doctoral Degree. Fort Collins: Colorado State University

[68] Venable N B H (2017). Hydroclimatological data and analyses from a headwaters region of Mongolia as boundary objects in interdisciplinary climate change research. Frontiers of Earth Science, 11: 457–468

[69] Wen R L, Xiao J L, Chang Z G, Zhai D Y, Xu Q H, Li Y C, Itoh S (2010). Holocene precipitation and temperature variations in the East Asian monsoonal margin from pollen data from Hulun Lake in northeastern Inner Mongolia, China. Boreas, 39(2): 262–272

[70] Yan Z, Jones P D, Davies T D, Moberg A, Bergström H, Camuffo D, Cocheo C, Maugeri M, Demarée G R, Verhoeve T, Thoen E, Barriendos M, Rodríguez R, Martín-Vide J, Yang C (2002). Trends of extreme temperatures in Europe and China based on daily observation. Clim Change, 53(1/3): 355–392

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