Can we stop global climate change? Does human scientific power reach the world's climate change? How do researchers respond?

As you know, humans are very intelligent and can predict the future climate of the world with hydrology, climatology and paleontology. But don't countries, especially industrialized countries, that produce the most harmful gases in the earth's atmosphere and think about the future of the earth's atmosphere? Do they listen to the research of climatologists? What would have to happen to force them to listen to climate scientists?

Miloud Chakit added a reply

Climate change is an important and complex global challenge, and scientific theories about it are based on extensive research and evidence. The future path of the world depends on various factors including human actions, political decisions and international cooperation.

Efforts to mitigate and adapt to climate change continue. While complete reversal may be challenging, important steps can be taken to slow progression and lessen its effects. This requires global cooperation, sustainable practices and the development and implementation of clean energy technologies.

Human scientific abilities play an important role, but dealing with climate change also requires social, economic and political changes. The goal is to limit global warming and its associated impacts, and collective action at the local, national, and international levels is essential for a more sustainable future.

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Osama Bahnas added a reply

It is impossible to stop global climate change. The human scientific power can not reach the world's climate change.

Borys Kapochkin added a reply

Mathematical models of increasing planetary temperature as a function of the argument - anthropogenic influence - are erroneous.

Alastair Bain McDonald added a reply

We could stop climate change but we won't! We have the scientific knowldge but not the political will. One could blame Russia and China from refusing to cooperate but half the population of the USA (Republicans) deny climate change is a problem and prefer their profligate life styles reply:

All climate change has been loaded on the CO2 responsible for the greenhouse effect. Therefore, there must be scientific experiments from several independent scientific institutes worldwide to find out what the greenhouse impact is on various CO2 concentrations. Then, there must be a conference from a reliable, professional organization with the participation of all independent scientific institutions to establish standards on CO2 concentrations and propose political actions accordingly.

The second action that can be done is to plant as many trees and plants as possible to breathe the CO2 and free the oxygen. Stop any deforestation and plant trees immediately in any bunt areas.

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Effect of Injecting Hydrogen Peroxide into Heavy Clay Loam Soil on Plant Water Status, NET CO2 Assimilation, Biomass, and Vascular Anatomy of Avocado Trees

In Chile, avocado (Persea americana Mill.) orchards are often located in poorly drained, low-oxygen soils, situation which limits fruit production and quality. The objective of this study was to evaluate the effect of injecting soil with hydrogen peroxide (H2O2) as a source of molecular oxygen, on plant water status, net CO2 assimilation, biomass and anatomy of avocado trees set in clay loam soil with water content maintained at field capacity. Three-year-old ‘Hass’ avocado trees were planted outdoors in containers filled with heavy loam clay soil with moisture content sustained at field capacity. Plants were divided into two treatments, (a) H2O2 injected into the soil through subsurface drip irrigation and (b) soil with no H2O2 added (control). Stem and root vascular anatomical characteristics were determined for plants in each treatment in addition to physical soil characteristics, net CO2 assimilation (A), transpiration (T), stomatal conductance (gs), stem water potential (SWP), shoot and root biomass, water use efficiency (plant biomass per water applied [WUEb]). Injecting H2O2 into the soil significantly increased the biomass of the aerial portions of the plant and WUEb, but had no significant effect on measured A, T, gs, or SWP. Xylem vessel diameter and xylem/phloem ratio tended to be greater for trees in soil injected with H2O2 than for controls. The increased biomass of the aerial portions of plants in treated soil indicates that injecting H2O2 into heavy loam clay soils may be a useful management tool in poorly aerated soil.

Shade trees reduce building energy use and CO2 emissions from power plants

Urban shade trees offer significant benefits in reducing building air-conditioning demand and improving urban air quality by reducing smog. The savings associated with these benefits vary by climate region and can be up to $200 per tree. The cost of planting trees and maintaining them can vary from $10 to $500 per tree. Tree-planting programs can be designed to have lower costs so that they offer potential savings to communities that plant trees. Our calculations suggest that urban trees play a major role in sequestering CO2 and thereby delay global warming. We estimate that a tree planted in Los Angeles avoids the combustion of 18 kg of carbon annually, even though it sequesters only 4.5-11 kg (as it would if growing in a forest). In this sense, one shade tree in Los Angeles is equivalent to three to five forest trees. In a recent analysis for Baton Rouge, Sacramento, and Salt Lake City, we estimated that planting an average of four shade trees per house (each with a top view cross section of 50 m2) would lead to an annual reduction in carbon emissions from power plants of 16,000, 41,000, and 9000 t, respectively (the per-tree reduction in carbon emissions is about 10-11 kg per year). These reductions only account for the direct reduction in the net cooling- and heating-energy use of buildings. Once the impact of the community cooling is included, these savings are increased by at least 25%.

Can Moisture-Indicating Understory Plants Be Used to Predict Survivorship of Large Lodgepole Pine Trees During Severe Outbreaks of Mountain Pine Beetle?

Why do some mature lodgepole pines survive mountain pine beetle outbreaks while most are killed? Here we test the hypothesis that mature trees growing in sites with vascular plant indicators of high relative soil moisture are more likely to survive mountain pine beetle outbreaks than mature trees associated with indicators of lower relative soil moisture. Working in the Clearwater Valley of south central British Columbia, we inventoried understory plants growing near large-diameter and small-diameter survivors and nonsurvivors of a mountain pine beetle outbreak in the mid-2000s. When key understory species were ranked according to their accepted soil moisture indicator value, a significant positive correlation was found between survivorship in large-diameter pine and inferred relative high soil moisture status—a finding consistent with the well-documented importance of soil moisture in the mobilization of defense compounds in lodgepole pine. We suggest that indicators of soil moisture may be useful in predicting the survival of large pine trees in future pine beetle outbreaks. Study Implications: A recent outbreak of the mountain pine beetle resulted in unprecedented levels of lodgepole pine mortality across southern inland British Columbia. Here, we use moisture-dependent understory plants to show that large lodgepole pine trees growing in sites with high relative moisture are more likely than similar trees in drier sites to survive severe outbreaks of mountain pine beetle—a finding that may be related to a superior ability to mobilize chemical defense compounds compared with drought-stressed trees.

Can Functional Traits Explain Plant Coexistence? A Case Study with Tropical Lianas and Trees

Organisms are adapted to their environment through a suite of anatomical, morphological, and physiological traits. These functional traits are commonly thought to determine an organism’s tolerance to environmental conditions. However, the differences in functional traits among co-occurring species, and whether trait differences mediate competition and coexistence is still poorly understood. Here we review studies comparing functional traits in two co-occurring tropical woody plant guilds, lianas and trees, to understand whether competing plant guilds differ in functional traits and how these differences may help to explain tropical woody plant coexistence. We examined 36 separate studies that compared a total of 140 different functional traits of co-occurring lianas and trees. We conducted a meta-analysis for ten of these functional traits, those that were present in at least five studies. We found that the mean trait value between lianas and trees differed significantly in four of the ten functional traits. Lianas differed from trees mainly in functional traits related to a faster resource acquisition life history strategy. However, the lack of difference in the remaining six functional traits indicates that lianas are not restricted to the fast end of the plant life–history continuum. Differences in functional traits between lianas and trees suggest these plant guilds may coexist in tropical forests by specializing in different life–history strategies, but there is still a significant overlap in the life–history strategies between these two competing guilds.

The use of operator action event trees to improve plant-specific emergency operating procedures

Even with plant standardization and generic emergency procedure guidelines (EPGs), there are sufficient dissimilarities in nuclear power plants that implementation of the guidelines at each plant must be performed in a manner that ensures consideration of plant-specific design features and operating characteristics. The use of operator action event tress (OAETs) results in identification of key features unique to each plant and yields insights into accident prevention and mitigation that can be factored into plant-specific emergency procedures. Operator action event trees were developed as a logical extension of the event trees developed during probabilistic risk analyses. The dominant accident sequences developed from a plant-specific probabilistic risk assessment represent the utility's best understanding of the most likely combination of events that must occur to create a situation in which core cooling is threatened or significant releases occur. It is desirable that emergency operating procedures (EOPs) provide adequate guidance leading to appropriate operator actions for these sequences. The OAETs provide a structured approach for assuring that the EOPs address these situations.

Plant and Wood Area Index of Solitary Trees for Urban Contexts in Nordic Cities

Background: We present the plant area index (PAI) measurements taken for 63 deciduous broadleaved tree species and 1 deciduous conifer tree species suitable for urban areas in Nordic cities. The aim was to evaluate PAI and wood area index (WAI) of solitary-grown broadleaved tree species and cultivars of the same age in order to present a data resource of individual tree characteristics viewed in summer (PAI) and in winter (WAI). Methods: All trees were planted as individuals in 2001 at the Hørsholm Arboretum in Denmark. The field method included a Digital Plant Canopy Imager where each scan and contrast values were set to consistent values. Results: The results illustrate that solitary trees differ widely in their WAI and PAI and reflect the integrated effects of leaf material and the woody component of tree crowns. The indications also show highly significant (P < 0.001) differences between species and genotypes. The WAI had an overall mean of 0.91 (± 0.03), ranging from Tilia platyphyllos ‘Orebro’ with a WAI of 0.32 (± 0.04) to Carpinus betulus ‘Fastigiata’ with a WAI of 1.94 (± 0.09). The lowest mean PAI in the dataset was Fraxinus angustifolia ‘Raywood’ with a PAI of 1.93 (± 0.05), whereas Acer campestre ‘Kuglennar’ represents the cultivar with the largest PAI of 8.15 (± 0.14). Conclusions: Understanding how this variation in crown architectural structure changes over the year can be applied to climate responsive design and microclimate modeling where plant and wood area index of solitary-grown trees in urban contexts are of interest.

Do Exotic Trees Threaten Southern Arid Areas of Tunisia? A Case Study Indian Journal of Ecology (2020) 00(0): 000-000 Plant-plant interactions

an afforested steppe planted This study was conducted in with aims to compare the effects of exotic and native Stipa tenacissima trees (and , respectively) on the understory vegetation and soil properties. For each tree species, two sub-Acacia salicina Pinus halepensis habitats were distinguished: the canopied sub-habitat (under the tree crown) and the un-canopied sub-habitat (open grassland). Soil moisture was measured in both sub-habitats at 10 cm depth. In parallel to soil moisture, investigated the effect of tree species on soil fertility. Soil samples were collected from the upper 10 cm soil, excluding litter and stones. The nutrient status of soil (organic matter, total N, extractable P) was significantly higher under compared to and open areas. This tendency remained constant with the soil water A. salicina P. halepensis content which was significantly higher under trees compared to open sub-habitats. For water content, there were no significant differences between studied trees. Total plant cover, species richness and the density of perennial species were significantly higher under the exotic species compared to other sub-habitats. Among the two tree species, had the strongest positive effect on the understory Acacia salicina vegetation. It seems to be more useful as a restoration tool in arid areas and more suitable to create islands of resources and foster succession than the other investigated tree species.

Effects of Elevated Atmospheric CO2 on Microbial Community Structure at the Plant-Soil Interface of Young Beech Trees (Fagus sylvatica L.) Grown at Two Sites with Contrasting Climatic Conditions

Soil microbial community responses to elevated atmospheric CO2 concentrations (eCO2) occur mainly indirectly via CO2-induced plant growth stimulation leading to quantitative as well as qualitative changes in rhizodeposition and plant litter. In order to gain insight into short-term, site-specific effects of eCO2 on the microbial community structure at the plant-soil interface, young beech trees (Fagus sylvatica L.) from two opposing mountainous slopes with contrasting climatic conditions were incubated under ambient (360 ppm) CO2 concentrations in a greenhouse. One week before harvest, half of the trees were incubated for 2 days under eCO2 (1,100 ppm) conditions. Shifts in the microbial community structure in the adhering soil as well as in the root rhizosphere complex (RRC) were investigated via TRFLP and 454 pyrosequencing based on 16S ribosomal RNA (rRNA) genes. Multivariate analysis of the community profiles showed clear changes of microbial community structure between plants grown under ambient and elevated CO2 mainly in RRC. Both TRFLP and 454 pyrosequencing showed a significant decrease in the microbial diversity and evenness as a response of CO2 enrichment. While Alphaproteobacteria dominated by Rhizobiales decreased at eCO2, Betaproteobacteria, mainly Burkholderiales, remained unaffected. In contrast, Gammaproteobacteria and Deltaproteobacteria, predominated by Pseudomonadales and Myxococcales, respectively, increased at eCO2. Members of the order Actinomycetales increased, whereas within the phylum Acidobacteria subgroup Gp1 decreased, and the subgroups Gp4 and Gp6 increased under atmospheric CO2 enrichment. Moreover, Planctomycetes and Firmicutes, mainly members of Bacilli, increased under eCO2. Overall, the effect intensity of eCO2 on soil microbial communities was dependent on the distance to the roots. This effect was consistent for all trees under investigation; a site-specific effect of eCO2 in response to the origin of the trees was not observed.

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Michael Senteza added a reply

We have to separate science from business and politics in the first place , before we can adequately discuss the resolution of this global challenge .

The considerations to global warming can be logically broken down in the following

1. What are the factors that have affected the earths climate over the last million years ? 100,000 years , 10,000 years and 1,000 years .

2. Observations , the climatic changes , formations , and archaeological data to support the changes

3. The actualities of the earth dynamics , for example we know that approx 2/3 of the earth is water and we also know that of the 1/3 we have approximately 60% un inhabitable , and the 40% habitable has approximately 10% who contribute to the alleged pollution , where for example as of 2022 (https://www.whichcar.com.au/news/how-many-cars-are-there-in-the-world) The US had 290 Million cars compared to Africa (50+ Countries ) 26 Million cars the EU (33 + countries ) 413 million cars then Asia pacific with 543 Million cars ( with a population of close to 2 billion ) . We estimate that as of may there are 1.45 billion cars . this means that North America , Western Europe and Asia pacific combined have approx 1.3 billion cars , and yet close to 70% of vegetation cover and forest space is concentrated in africa , south america , northern europe and canada. we need to analyse this

4. We need to also analyse the actualities of the cause separating factors outside our reach , for example global worming as opposed to climate change . We know that climate change which has been geologically and scientifically observed to have been the reason things like Oil came into place , species became extinct and other formations created . We need to realise that a fair share of changes in climate (which some times may be confused with global worming ) have been due to changes in the earth's rotation , axis and orbit around the sun . These are factors that greatly affect the distribution of the sun's radiation on to the surface of the earth and the atmospheric impact , them make consideration of how much we produce , the dispersion rate , natural chemical balances and volumetric analysis of concentration , assimilation and alteration of elements .

5. The extent to which non scientific factors are contributing to attenuating strength of scientific argument . It is not uncommon to have politicians alter the rhetoric to serve their agenda , however it's even worse when the sponsors of the scientific research are intent on achieving specific goals and not facts .

In conclusion humans are intelligent enough to either end of mitigation the impact of global worming if it can be detached from capitalism and politics . Science can and will provide answers