Integrating the effects of climate change on terrestrial ecosystems

2019 ◽

pp. 77-88

Author(s):

S. A. Lysenko

Keyword(s):

Climate Change ◽

Carbon Dioxide ◽

Vegetation Index ◽

Precipitation Amount ◽

Terrestrial Ecosystems ◽

Vegetation Period ◽

Climatic Trend ◽

Vegetation Growth ◽

Current Century ◽

The Impact

The spatial and temporal particularities of Normalized Differential Vegetation Index (NDVI) changes over territory of Belarus in the current century and their relationship with climate change were investigated. The rise of NDVI is observed at approximately 84% of the Belarus area. The statistically significant growth of NDVI has exhibited at nearly 35% of the studied area (t-test at 95% confidence interval), which are mainly forests and undeveloped areas. Croplands vegetation index is largely descending. The main factor of croplands bio-productivity interannual variability is precipitation amount in vegetation period. This factor determines more than 60% of the croplands NDVI dispersion. The long-term changes of NDVI could be explained by combination of two factors: photosynthesis intensifying action of carbon dioxide and vegetation growth suppressing action of air warming with almost unchanged precipitation amount. If the observed climatic trend continues the croplands bio-productivity in many Belarus regions could be decreased at more than 20% in comparison with 2000 year. The impact of climate change on the bio-productivity of undeveloped lands is only slightly noticed on the background of its growth in conditions of rising level of carbon dioxide in the atmosphere.

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Reduced resilience of terrestrial ecosystems locally is not reflected on a global scale

Communications Earth & Environment ◽

10.1038/s43247-021-00163-1 ◽

2021 ◽

Vol 2 (1) ◽

Author(s):

Yuhao Feng ◽

Haojie Su ◽

Zhiyao Tang ◽

Shaopeng Wang ◽

Xia Zhao ◽

...

Keyword(s):

Climate Change ◽

Global Climate Change ◽

Vegetation Index ◽

Global Climate ◽

Terrestrial Ecosystem ◽

Terrestrial Ecosystems ◽

Global Scale ◽

Ecological Resilience ◽

Terrestrial Vegetation ◽

Ecosystem Resilience

AbstractGlobal climate change likely alters the structure and function of vegetation and the stability of terrestrial ecosystems. It is therefore important to assess the factors controlling ecosystem resilience from local to global scales. Here we assess terrestrial vegetation resilience over the past 35 years using early warning indicators calculated from normalized difference vegetation index data. On a local scale we find that climate change reduced the resilience of ecosystems in 64.5% of the global terrestrial vegetated area. Temperature had a greater influence on vegetation resilience than precipitation, while climate mean state had a greater influence than climate variability. However, there is no evidence for decreased ecological resilience on larger scales. Instead, climate warming increased spatial asynchrony of vegetation which buffered the global-scale impacts on resilience. We suggest that the response of terrestrial ecosystem resilience to global climate change is scale-dependent and influenced by spatial asynchrony on the global scale.

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A coupled multi-proxy and process modelling approach for extraction of quantitative terrestrial ecosystem information from speleothems

10.5194/egusphere-egu21-4761 ◽

2021 ◽

Author(s):

Franziska Lechleitner ◽

Christopher C. Day ◽

Oliver Kost ◽

Micah Wilhelm ◽

Negar Haghipour ◽

...

Keyword(s):

Climate Change ◽

Soil Respiration ◽

Western Europe ◽

Global Climate ◽

Terrestrial Ecosystem ◽

Terrestrial Ecosystems ◽

Clear Correlation ◽

Northern Spain ◽

Regional Temperature ◽

Global Carbon

Terrestrial ecosystems are intimately linked with the global climate system, but their response to ongoing and future anthropogenic climate change remains poorly understood. Reconstructing the response of terrestrial ecosystem processes over past periods of rapid and substantial climate change can serve as a tool to better constrain the sensitivity in the ecosystem-climate response.In this talk, we will present a new reconstruction of soil respiration in the temperate region of Western Europe based on speleothem carbon isotopes (&#948;13C). Soil respiration remains poorly constrained over past climatic transitions, but is critical for understanding the global carbon cycle and its response to ongoing anthropogenic warming. Our study builds upon two decades of speleothem research in Western Europe, which has shown clear correlation between &#948;13C and regional temperature reconstructions during the last glacial and the deglaciation, with exceptional regional coherency in timing, amplitude, and absolute &#948;13C variation. By combining innovative multi-proxy geochemical analysis (&#948;13C, Ca isotopes, and radiocarbon) on three speleothems from Northern Spain, and quantitative forward modelling of processes in soil, karst, and cave, we show how deglacial variability in speleothem &#948;13C is best explained by increasing soil respiration. Our study is the first to quantify and remove the effects of prior calcite precipitation (PCP, using Ca isotopes) and bedrock dissolution (open vs closed system, using the radiocarbon reservoir effect) from the speleothem &#948;13C signal to derive changes in respired &#948;13C over time. Our approach allows us to estimate the temperature sensitivity of soil respiration (Q10), which is higher than current measurements, suggesting that part of the speleothem signal may be related to a change in the composition of the soil respired &#948;13C. This is likely related to changing substrate through increasing contribution from vegetation biomass with the onset of the Holocene.These results highlight the exciting possibilities speleothems offer as a coupled archive for quantitative proxy-based reconstructions of climate and ecosystem conditions.

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Soil–landform–plant-community relationships of a periglacial landscape on Potter Peninsula, maritime Antarctica

Solid Earth ◽

10.5194/se-6-583-2015 ◽

2015 ◽

Vol 6 (2) ◽

pp. 583-594 ◽

Cited By ~ 12

Author(s):

E. L. Poelking ◽

C. E. R. Schaefer ◽

E. I. Fernandes Filho ◽

A. M. de Andrade ◽

A. A. Spielmann

Keyword(s):

Climate Change ◽

Plant Communities ◽

Terrestrial Ecosystems ◽

Maritime Antarctica ◽

Climate Change Effects ◽

Ornithogenic Soils ◽

Physical Environmental Factors ◽

Potter Peninsula

Abstract. Integrated studies on the interplay between soils, periglacial geomorphology and plant communities are crucial for the understanding of climate change effects on terrestrial ecosystems of maritime Antarctica, one of the most sensitive areas to global warming. Knowledge on physical environmental factors that influence plant communities can greatly benefit studies on the monitoring of climate change in maritime Antarctica, where new ice-free areas are being constantly exposed, allowing plant growth and organic carbon inputs. The relationship between topography, plant communities and soils was investigated on Potter Peninsula, King George Island, maritime Antarctica. We mapped the occurrence and distribution of plant communities and identified soil–landform–vegetation relationships. The vegetation map was obtained by classification of a QuickBird image, coupled with detailed landform and characterization of 18 soil profiles. The sub-formations were identified and classified, and we also determined the total elemental composition of lichens, mosses and grasses. Plant communities on Potter Peninsula occupy 23% of the ice-free area, at different landscape positions, showing decreasing diversity and biomass from the coastal zone to inland areas where sub-desert conditions prevail. There is a clear dependency between landform and vegetated soils. Soils that have greater moisture or are poorly drained, and with acid to neutral pH, are favourable for moss sub-formations. Saline, organic-matter-rich ornithogenic soils of former penguin rookeries have greater biomass and diversity, with mixed associations of mosses and grasses, while stable felsenmeers and flat rocky cryoplanation surfaces are the preferred sites for Usnea and Himantormia lugubris lichens at the highest surface. Lichens sub-formations cover the largest vegetated area, showing varying associations with mosses.

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What the past can say about the present and future of fire

Quaternary Research ◽

10.1017/qua.2020.48 ◽

2020 ◽

Vol 96 ◽

pp. 66-87

Author(s):

Jennifer R. Marlon

Keyword(s):

Climate Change ◽

Terrestrial Ecosystems ◽

Combustion Products ◽

Temperature Changes ◽

The Public ◽

The Past ◽

Warming Climate ◽

Highly Sensitive ◽

In Fire ◽

Very High

AbstractWildfires are an integral part of most terrestrial ecosystems. Paleofire records composed of charcoal, soot, and other combustion products deposited in lake and marine sediments, soils, and ice provide a record of the varying importance of fire over time on every continent. This study reviews paleofire research to identify lessons about the nature of fire on Earth and how its past variability is relevant to modern environmental challenges. Four lessons are identified. First, fire is highly sensitive to climate change, and specifically to temperature changes. As long as there is abundant, dry fuel, we can expect that in a warming climate, fires will continue to grow unusually large, severe, and uncontrollable in fire-prone environments. Second, a better understanding of “slow” (interannual to multidecadal) socioecological processes is essential for predicting future wildfire and carbon emissions. Third, current patterns of burning, which are very low in some areas and very high in others—are often unprecedented in the context of the Holocene. Taken together, these insights point to a fourth lesson—that current changes in wildfire dynamics provide an opportunity for paleoecologists to engage the public and help them understand the potential consequences of anthropogenic climate change.

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Changes in Soil Carbon Sequestration during Woody Plant Encroachment in Arid Ecosystems

Plantae Scientia ◽

10.32439/ps.v4i4-5.266-276 ◽

2021 ◽

Vol 4 (4-5) ◽

pp. 266-276

Author(s):

Pratap Naikwade

Keyword(s):

Climate Change ◽

Carbon Sequestration ◽

Soil Carbon ◽

Atmospheric Carbon Dioxide ◽

Global Climate ◽

Terrestrial Ecosystems ◽

Greenhouse Gas Mitigation ◽

Arid Ecosystems ◽

Woody Encroachment ◽

Organic C

Carbon sequestration is one of the most important and highly recommended measures for mitigating climate change. Soil organic carbon (SOC) has potential to sequester the largest amount of carbon (C) for the longest time period in the midst of the organic C sinks in terrestrial ecosystems of the earth. In recent years, apprehension of the role of soils as sink for carbon on a wide-ranging scale has become dynamic. From last 150 years, encroachment of trees and shrubs into grasslands and the ‘thicketization’ of savannas have been reported and is a global phenomenon. One possibly beneficial effect could be that the shrub and tree-dominated ecosystems will sequester more carbon and will be a buffer for elevated atmospheric carbon dioxide (CO2) levels. The question of what is impact of woody encroachment on soil carbon balance of an ecosystem has proved difficult to answer, and the results remain debatable. The magnitude and pattern of changes in the SOC with woody encroachment are exceedingly abstruse and varies from significant increases, to significant decreases to no net change in SOC. Impact of wood plant encroachment on carbon sequestration is discussed in this paper considering various studies with different results so it will lead to better understanding of the complex phenomenon. SOC sequestration is effective greenhouse gas mitigation strategy and a vital ecosystem service. Increasing SOC may helpful to mitigate negative effects of growing concentration of CO2 in atmosphere and may be advantageous in decelerating or reversal in global climate change rate.

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Impacts of climate change on the terrestrial ecosystems of Madeira

International Journal of Design & Nature and Ecodynamics ◽

10.2495/dne-v4-n4-413-422 ◽

2010 ◽

Vol 4 (4) ◽

pp. 413-422 ◽

Cited By ~ 8

Author(s):

M.J. Cruz ◽

R. Aguiar ◽

A. Correia ◽

T. Tavares ◽

J.S. Pereira ◽

...

Keyword(s):

Climate Change ◽

Terrestrial Ecosystems ◽

Impacts Of Climate Change

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Tracking vegetation phenology across diverse North American biomes using PhenoCam imagery

Scientific Data ◽

10.1038/sdata.2018.28 ◽

2018 ◽

Vol 5 (1) ◽

Cited By ~ 110

Author(s):

Andrew D. Richardson ◽

Koen Hufkens ◽

Tom Milliman ◽

Donald M. Aubrecht ◽

Min Chen ◽

...

Keyword(s):

Climate Change ◽

Vegetation Type ◽

Digital Camera ◽

Region Of Interest ◽

Remote Sensing Data ◽

Climate Change Impacts ◽

Terrestrial Ecosystems ◽

Vegetation Phenology ◽

Phenological Model ◽

Vegetation Activity

Abstract Vegetation phenology controls the seasonality of many ecosystem processes, as well as numerous biosphere-atmosphere feedbacks. Phenology is also highly sensitive to climate change and variability. Here we present a series of datasets, together consisting of almost 750 years of observations, characterizing vegetation phenology in diverse ecosystems across North America. Our data are derived from conventional, visible-wavelength, automated digital camera imagery collected through the PhenoCam network. For each archived image, we extracted RGB (red, green, blue) colour channel information, with means and other statistics calculated across a region-of-interest (ROI) delineating a specific vegetation type. From the high-frequency (typically, 30 min) imagery, we derived time series characterizing vegetation colour, including “canopy greenness”, processed to 1- and 3-day intervals. For ecosystems with one or more annual cycles of vegetation activity, we provide estimates, with uncertainties, for the start of the “greenness rising” and end of the “greenness falling” stages. The database can be used for phenological model validation and development, evaluation of satellite remote sensing data products, benchmarking earth system models, and studies of climate change impacts on terrestrial ecosystems.

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