Climatic changes are altering Earth's hydrological cycle, resulting in altered precipitation amounts, increased interannual variability of precipitation, and more frequent extreme precipitation events. These trends will likely continue into the future, having substantial impacts on net primary productivity (
Rangelands are Earth's dominant land cover and are important providers of ecosystem services. Reliance on rangelands is projected to grow, thus understanding the sensitivity of rangelands to future climates is essential. We used a new ecosystem model of moderate complexity that allows, for the first time, to quantify global changes expected in rangelands under future climates. The mean global annual net primary production (
- NSF-PAR ID:
- 10048606
- Publisher / Repository:
- Wiley-Blackwell
- Date Published:
- Journal Name:
- Global Change Biology
- Volume:
- 24
- Issue:
- 3
- ISSN:
- 1354-1013
- Page Range / eLocation ID:
- p. 1382-1393
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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Abstract NPP ) and associated ecosystem services such as food production and carbon sequestration. Frequently, experimental manipulations of precipitation have linked altered precipitation regimes to changes inNPP . Yet, findings have been diverse and substantial uncertainty still surrounds generalities describing patterns of ecosystem sensitivity to altered precipitation. Additionally, we do not know whether previously observed correlations betweenNPP and precipitation remain accurate when precipitation changes become extreme. We synthesized results from 83 case studies of experimental precipitation manipulations in grasslands worldwide. We used meta‐analytical techniques to search for generalities and asymmetries of abovegroundNPP (ANPP ) and belowgroundNPP (BNPP ) responses to both the direction and magnitude of precipitation change. Sensitivity (i.e., productivity response standardized by the amount of precipitation change) ofBNPP was similar under precipitation additions and reductions, butANPP was more sensitive to precipitation additions than reductions; this was especially evident in drier ecosystems. Additionally, overall relationships between the magnitude of productivity responses and the magnitude of precipitation change were saturating in form. The saturating form of this relationship was likely driven byANPP responses to very extreme precipitation increases, although there were limited studies imposing extreme precipitation change, and there was considerable variation among experiments. This highlights the importance of incorporating gradients of manipulations, ranging from extreme drought to extreme precipitation increases into future climate change experiments. Additionally, policy and land management decisions related to global change scenarios should consider howANPP andBNPP responses may differ, and that ecosystem responses to extreme events might not be predicted from relationships found under moderate environmental changes. -
Abstract In semiarid regions, vegetation constraints on plant growth responses to precipitation (
PPT ) are hypothesized to place an upper limit on net primary productivity (NPP ), leading to predictions of future shifts from currently defined linear to saturatingNPP –PPT relationships as increases in both dry and wetPPT extremes occur. We experimentally tested this prediction by imposing a replicated gradient of growing seasonPPT (GSP ,n = 11 levels,n = 4 replicates), ranging from the driest to wettest conditions in the 75‐yr climate record, within a semiarid grassland. We focused on responses of two key ecosystem processes: abovegroundNPP (ANPP ) and soil respiration (R s).ANPP andR sboth exhibited greater relative responses to wet vs. dryGSP extremes, with a linear relationship consistently best explaining the response of both processes toGSP . However, this responsiveness toGSP peaked at moderate levels of extremity for both processes, and declined at the most extremeGSP levels, suggesting that greater sensitivity ofANPP andR sto wet vs. dry conditions may diminish under increased magnitudes ofGSP extremes. Underlying these responses was rapid plant compositional change driven by increased forb production and cover asGSP transitioned to extreme wet conditions. This compositional shift increased the magnitude ofANPP responses to wetGSP extremes, as well as the slope and variability explained in theANPP –GSP relationship. Our findings suggest that rapid plant compositional change may act as a mediator of semiarid ecosystem responses to predicted changes inGSP extremes. -
Abstract Soils are an important source of
NO , particularly in dry lands because of trade‐offs that develop between biotic and abioticNO ‐producing processes when soils dry out. Understanding how drier climates may offset the balance of these trade‐offs as soils transition toward more arid states is, therefore, critical to estimating globalNO budgets, especially because drylands are expected to increase in size. We measuredNO emission pulses after wetting soils from similar lithologies along an altitudinal gradient in the Sierra Nevada,CA , where mean annual precipitation varied from 670 to 1500 mm. Along the gradient, we measured fieldNO emissions, and used chloroform in the laboratory to reduce microbial activity and partition between biotic and abioticNO ‐producing processes (i.e., chemodenitrification). FieldNO emission pulses were lowest in the acidic andSOM ‐rich soils (4–72 ngNO ‐N m−2s−1), but were highest in the high‐elevation barren site (~560 ngNO ‐N m−2s−1). In the laboratory,NO emission pulses were up to 19× greater in chloroform‐treated soils than in the controls, and these abiotic pulses increased with elevation aspH decreased (6.2–4.4) and soil organic matter (SOM ) increased (18–157 mg C g−1). Drought can shift the balance between the biotic and abiotic processes that produceNO , favoring chemodenitrification during periods when biological processes become stressed. Acidic andSOM ‐rich soils, which typically develop under mesic conditions, are most vulnerable to N loss viaNO as interactions betweenpH ,SOM , and drought stimulate chemodenitrification. -
Abstract Savanna ecosystems contribute ~30% of global net primary production (
NPP ), but they vary substantially in composition and function, specifically in the understory, which can result in complex responses to environmental fluctuations. We tested how understory phenology and its contribution to ecosystem productivity within a longleaf pine ecosystem varied at two ends of a soil moisture gradient (mesic and xeric). We used the Normalized Difference Vegetation Index (NDVI ) of the understory and ecosystem productivity estimates from eddy covariance systems to understand how variation in the understory affected overall ecosystem recovery from disturbances (drought and fire). We found that the mesic site recovered more rapidly from the disturbance of fire, compared to the xeric site, indicated by a faster increase inNDVI . During drought, understoryNDVI at the xeric site decreased less compared to the mesic site, suggesting adaptation to lower soil moisture conditions. Our results also show large variation within savanna ecosystems in the contribution of the understory to ecosystem productivity and recovery, highlighting the critical need to further subcategorize global savanna ecosystems by their structural features, to accurately predict their contribution to global estimates ofNPP . -
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