Impact of Varying Storm Intensity and Consecutive Dry Days on Grassland Soil Moisture

Intra-annual precipitation patterns are expected to shift toward more intense storms and longer dry periods because of changes in climate within future decades. Using satellite-derived estimates of plant growth combined with in situ measurements of precipitation and soil moisture between 1999 and 2013, this study quantifiedthe relationship between intra-annual precipitation patterns, annual average soil moisture (at 5-cm depth), and plant growth at nine grassland sites across the southern United States. Results showed a fundamental difference in the response to varying precipitation patterns between mesic and semiarid grasslands. Surface soil moisture in mesic grasslands decreased with an increase of high-intensity storms, whereas in semiarid grasslands, soil moisture decreased with longer dry periods. For these sites, annual average soil moisture was a better indicator of grassland production than total annual precipitation. This improved ability to predict variability in soil moisture and plant growth with changing hydroclimatic conditions will result in more efficient resource management and better-informed policy decisions.

[1]  Yann Kerr,et al.  SMOS: The Mission and the System , 2008, IEEE Transactions on Geoscience and Remote Sensing.

[2]  G. MacDonald,et al.  Water, climate change, and sustainability in the southwest , 2010, Proceedings of the National Academy of Sciences.

[3]  A. Knapp,et al.  Variation among biomes in temporal dynamics of aboveground primary production. , 2001, Science.

[4]  M. Dore Climate change and changes in global precipitation patterns: what do we know? , 2005, Environment international.

[5]  Mark S. Seyfried,et al.  Dielectric Loss and Calibration of the Hydra Probe Soil Water Sensor , 2005 .

[6]  M. Haylock,et al.  Observed coherent changes in climatic extremes during the second half of the twentieth century , 2002 .

[7]  Alfredo Huete,et al.  Extreme precipitation patterns and reductions of terrestrial ecosystem production across biomes , 2013 .

[8]  Wenzhi Zhao,et al.  The response of soil moisture to rainfall event size in subalpine grassland and meadows in a semi-arid mountain range: A case study in northwestern China’s Qilian Mountains , 2012 .

[9]  Alfredo Huete,et al.  Functional response of U.S. grasslands to the early 21st-century drought. , 2014, Ecology.

[10]  Delphis F. Levia,et al.  Soil moisture: A central and unifying theme in physical geography , 2011 .

[11]  Markus Reichstein,et al.  Consequences of More Extreme Precipitation Regimes for Terrestrial Ecosystems , 2008 .

[12]  M. Jankju Individual Performances and the Interaction Between Arid Land Plants Affected by the Growth Season Water Pulses , 2008 .

[13]  Yann Kerr,et al.  Soil Moisture , 1922, Botanical Gazette.

[14]  G. Meehl,et al.  Climate extremes: observations, modeling, and impacts. , 2000, Science.

[15]  J. Holmes,et al.  DIGESTIBILITY OF ALPINE PASTURE ON THE BOGONG HIGH PLAINS OF VICTORIA , 1986 .

[16]  N. Kiang,et al.  How plant functional-type, weather, seasonal drought, and soil physical properties alter water and energy fluxes of an oak-grass savanna and an annual grassland , 2004 .

[17]  A. Huete,et al.  Overview of the radiometric and biophysical performance of the MODIS vegetation indices , 2002 .

[18]  Yann Kerr,et al.  Soil moisture retrieval from space: the Soil Moisture and Ocean Salinity (SMOS) mission , 2001, IEEE Trans. Geosci. Remote. Sens..

[19]  M. Power,et al.  Species Interactions Reverse Grassland Responses to Changing Climate , 2007, Science.

[20]  A. Holtslag,et al.  Influence of Soil Moisture on Boundary Layer Cloud Development , 2004 .

[21]  D. Lawrence,et al.  Regions of Strong Coupling Between Soil Moisture and Precipitation , 2004, Science.

[22]  J. Blair,et al.  Rainfall Variability, Carbon Cycling, and Plant Species Diversity in a Mesic Grassland , 2002, Science.

[23]  A. Knapp,et al.  Increasing precipitation event size increases aboveground net primary productivity in a semi-arid grassland , 2008, Oecologia.

[24]  P. Blanken,et al.  An underestimated role of precipitation frequency in regulating summer soil moisture , 2012 .

[25]  Per Jönsson,et al.  TIMESAT - a program for analyzing time-series of satellite sensor data , 2004, Comput. Geosci..

[26]  M. S. Moran,et al.  Ecosystem resilience despite large-scale altered hydroclimatic conditions , 2013, Nature.

[27]  Dawn M. Kaufman,et al.  Changes in grassland ecosystem function due to extreme rainfall events: implications for responses to climate change , 2008 .

[28]  Fabio Castelli,et al.  Mutual interaction of soil moisture state and atmospheric processes , 1996 .

[29]  Jiancheng Shi,et al.  The Soil Moisture Active Passive (SMAP) Mission , 2010, Proceedings of the IEEE.

[30]  J. Blair,et al.  Contingent productivity responses to more extreme rainfall regimes across a grassland biome , 2009 .

[31]  A. Knapp,et al.  Unexpected patterns of sensitivity to drought in three semi-arid grasslands , 2012, Oecologia.

[32]  Christopher B. Field,et al.  Grassland Responses to Global Environmental Changes Suppressed by Elevated CO2 , 2002, Science.

[33]  Matthias Drusch,et al.  Global Automated Quality Control of In Situ Soil Moisture Data from the International Soil Moisture Network , 2013 .

[34]  Shaopeng Wang,et al.  Soil Respiration in Tibetan Alpine Grasslands: Belowground Biomass and Soil Moisture, but Not Soil Temperature, Best Explain the Large-Scale Patterns , 2012, PloS one.

[35]  K. Renard,et al.  Biomass distribution at grassland and shrubland sites. , 1986 .

[36]  J. M. Schneider,et al.  Spatiotemporal Variations in Soil Water: First Results from the ARM SGP CART Network , 2003 .