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Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
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The experimental conditions in a gravimetric analysis should be optimized to maximize the particle size and purity of the obtained precipitate. Ideally, the concentration of the precipitating reagent should be low with effective stirring to maintain low relative supersaturation for the growth of large crystals. In homogeneous precipitation, the precipitant is slowly generated by a chemical reaction in the solution to avoid local reagent excesses. For example, urea decomposes gradually to...
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Precipitation and coprecipitation methods can be used to separate a mixture of ions in a solution. In qualitative inorganic analysis, ions that form sparingly soluble precipitates with the same reagent are separated based on the differences in solubility products. For example, consider the separation of Cu(II) and Fe(II) ions by precipitation as insoluble sulfides. First, copper(II) sulfide is precipitated by the addition of acidic H2S, where the dissociation of H2S is suppressed. Adding H2S...
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Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
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Using Generative Art to Convey Past and Future Climate Transitions
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Predicting future climate at high spatial and temporal resolution.

Ilya M D Maclean1

  • 1Environment and Sustainability Institute, University of Exeter, Penryn, UK.

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|October 23, 2019
PubMed
Summary
This summary is machine-generated.

Future climate change impacts on organisms require fine-grained microclimate data. This study provides methods for hourly temperature and soil moisture estimates, revealing less extreme future conditions than previously thought.

Keywords:
ecologymechanistic modelmicroclimatesoil moisturesoil temperaturespecies distributions

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Area of Science:

  • Ecology
  • Climate Science
  • Environmental Modeling

Background:

  • Current climate change studies often use coarse, seasonally aggregated data, masking vital microclimate variability.
  • This approach inadequately represents the actual environmental conditions organisms face in the wild.
  • A significant gap exists in understanding fine-resolution climatic changes and their biological implications.

Purpose of the Study:

  • To present methods for generating fine-grained, hourly microclimate estimates (temperature and soil moisture) over decadal timescales.
  • To improve the accuracy of predicting future climatic conditions experienced by organisms.
  • To provide tools for biologists to assess climate change impacts at a relevant scale.

Main Methods:

  • Disaggregation of coarse climate data to hourly resolution to drive physical microclimate models.
  • Incorporation of mesoclimatic effects (e.g., elevation, coastal exposure) and local factors (terrain, vegetation) using energy balance and hydrological equations.
  • Development of R packages to process data and run thermal and hydrological microclimate models.

Main Results:

  • Application of the methods to the Lizard Peninsula, UK, yielded hourly temperature estimates at high spatial resolution.
  • Fine-resolution variability in climatic changes was observed, driven by landscape-climate interactions.
  • Future extreme climatic conditions were predicted to be less novel than those estimated using aggregated data.

Conclusions:

  • Accurate microclimate modeling is crucial for understanding organismal responses to climate change.
  • The developed methods and tools enable more realistic assessments of future environmental conditions.
  • This approach highlights the importance of fine-scale data for ecological predictions.