Literature DB >> 26183431

Desert grassland responses to climate and soil moisture suggest divergent vulnerabilities across the southwestern United States.

Jennifer R Gremer1, John B Bradford1, Seth M Munson1, Michael C Duniway2.   

Abstract

Climate change predictions include warming and drying trends, which are expected to be particularly pronounced in the southwestern United States. In this region, grassland dynamics are tightly linked to available moisture, yet it has proven difficult to resolve what aspects of climate drive vegetation change. In part, this is because it is unclear how heterogeneity in soils affects plant responses to climate. Here, we combine climate and soil properties with a mechanistic soil water model to explain temporal fluctuations in perennial grass cover, quantify where and the degree to which incorporating soil water dynamics enhances our ability to understand temporal patterns, and explore the potential consequences of climate change by assessing future trajectories of important climate and soil water variables. Our analyses focused on long-term (20-56 years) perennial grass dynamics across the Colorado Plateau, Sonoran, and Chihuahuan Desert regions. Our results suggest that climate variability has negative effects on grass cover, and that precipitation subsidies that extend growing seasons are beneficial. Soil water metrics, including the number of dry days and availability of water from deeper (>30 cm) soil layers, explained additional grass cover variability. While individual climate variables were ranked as more important in explaining grass cover, collectively soil water accounted for 40-60% of the total explained variance. Soil water conditions were more useful for understanding the responses of C3 than C4 grass species. Projections of water balance variables under climate change indicate that conditions that currently support perennial grasses will be less common in the future, and these altered conditions will be more pronounced in the Chihuahuan Desert and Colorado Plateau. We conclude that incorporating multiple aspects of climate and accounting for soil variability can improve our ability to understand patterns, identify areas of vulnerability, and predict the future of desert grasslands. Published 2015. This article is a U.S. Government work and is in the public domain in the USA.

Keywords:  Chihuahuan Desert; Colorado Plateau; Sonoran Desert; arid and semiarid; climate change; climate variability; drought; soil water dynamics

Mesh:

Substances:

Year:  2015        PMID: 26183431     DOI: 10.1111/gcb.13043

Source DB:  PubMed          Journal:  Glob Chang Biol        ISSN: 1354-1013            Impact factor:   10.863


  3 in total

1.  Increasing temperature seasonality may overwhelm shifts in soil moisture to favor shrub over grass dominance in Colorado Plateau drylands.

Authors:  Jennifer R Gremer; Caitlin Andrews; Jodi R Norris; Lisa P Thomas; Seth M Munson; Michael C Duniway; John B Bradford
Journal:  Oecologia       Date:  2018-11-09       Impact factor: 3.225

2.  Decline in biological soil crust N-fixing lichens linked to increasing summertime temperatures.

Authors:  Rebecca Finger-Higgens; Michael C Duniway; Stephen Fick; Erika L Geiger; David L Hoover; Alix A Pfennigwerth; Matthew W Van Scoyoc; Jayne Belnap
Journal:  Proc Natl Acad Sci U S A       Date:  2022-04-11       Impact factor: 12.779

3.  Anthropogenic impacts drive niche and conservation metrics of a cryptic rattlesnake on the Colorado Plateau of western North America.

Authors:  M R Douglas; M A Davis; M Amarello; J J Smith; G W Schuett; H-W Herrmann; A T Holycross; M E Douglas
Journal:  R Soc Open Sci       Date:  2016-04-27       Impact factor: 2.963

  3 in total

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