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OpenStem
@openstem · Joined Jul 2026
7420 public items8 groups
Note~273 words · 1 min
The Linear Feedback Framework Climate sensitivity is quantified by linearizing the global top-of-atmosphere energy budget around an equilibrium state: ΔN is radiative imbalance, ΔF the applied forcing (e.g. from CO₂), ΔT the resulting globa
Environmental · L5 · Quantifying Earth System Feedbacks
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Environmental · L5 · Quantifying Earth System FeedbacksNote~309 words · 2 min
Governing Physics: The Richards Equation Water movement through the unsaturated (vadose) zone — between the land surface and the water table — is governed by the Richards equation, combining mass conservation with Darcy's law generalized to
Environmental · L5 · Hydrological Modeling: From Richards' Equation to Watershed Models
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Environmental · L5 · Hydrological Modeling: From Richards' Equation to Watershed ModelsNote~330 words · 2 min
Modeling the Dose-Response Curve A population's response to a toxicant (mortality, growth impairment, reproductive failure) typically follows a sigmoid curve against log-dose — few individuals respond at very low doses, most respond in a mi
Environmental · L5 · Quantitative Ecotoxicology and Risk Assessment
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Environmental · L5 · Quantitative Ecotoxicology and Risk AssessmentNote~266 words · 1 min
Atmospheric Correction: Inverting the Radiative Transfer Equation What a satellite sensor records — top-of-atmosphere (TOA) radiance — is not the true surface reflectance scientists usually want. Sunlight is scattered and absorbed traveling
Environmental · L5 · Remote Sensing Retrieval and Inversion
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Environmental · L5 · Remote Sensing Retrieval and InversionNote~359 words · 2 min
Integrated Assessment Models: Coupling Economy, Climate, and Damages An Integrated Assessment Model (IAM) links three sub-modules into a single framework for exploring climate-economy trade-offs: an economic module projecting growth and emi
Environmental · L5 · Integrated Assessment Models and the Social Cost of Carbon
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Environmental · L5 · Integrated Assessment Models and the Social Cost of CarbonNote~335 words · 2 min
Glen's Flow Law: Ice as a Non-Newtonian Fluid Glacial ice deforms under its own weight and applied stress according to a power-law rheology, not simple linear viscosity: Because n ≈ 3, deformation rate is highly sensitive to stress — small
Environmental · L5 · Ice Sheet Dynamics and Mass Balance
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Environmental · L5 · Ice Sheet Dynamics and Mass BalanceNote~339 words · 2 min
The Closure Problem Reynolds-averaging the governing fluid equations to separate mean flow from turbulent fluctuations introduces new unknown turbulent flux terms (Reynolds stresses, e.g. u'w') that have no equation of their own within the
Environmental · L5 · Boundary Layer Turbulence and Monin-Obukhov Similarity Theory
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Environmental · L5 · Boundary Layer Turbulence and Monin-Obukhov Similarity TheoryNote~319 words · 2 min
The Global Meteoric Water Line Stable isotopes of hydrogen (²H, or deuterium) and oxygen (¹⁸O) in the water molecule itself — not just dissolved tracers — fractionate together during evaporation and condensation in the hydrological cycle, p
Environmental · L5 · Isotope Hydrology: Tracing Water Sources and Ages
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Environmental · L5 · Isotope Hydrology: Tracing Water Sources and AgesNote~514 words · 3 min
What an SDM Actually Estimates A species distribution model fits a statistical relationship between known occurrence records and environmental predictor layers, producing a suitability surface used for conservation planning, invasive-specie
Environmental · L5 · Species Distribution Modeling: Niche Theory and Model Transferability
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Environmental · L5 · Species Distribution Modeling: Niche Theory and Model TransferabilityNote~362 words · 2 min
The Species Continuity Equation A chemical transport model (CTM) tracks pollutant concentration C(x,y,z,t) by solving a continuity equation on a 3D grid: transport by resolved winds, turbulent diffusion, chemical production/loss, emissions,
Environmental · L5 · Atmospheric Chemistry & Chemical Transport Modeling
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Environmental · L5 · Atmospheric Chemistry & Chemical Transport ModelingNote~386 words · 2 min
The Advection-Diffusion Equation Environmental fluid mechanics applies one governing equation — advection by the mean flow plus Fickian diffusion plus sources — across air, river, and groundwater contexts: In turbulent environmental flows,
Environmental · L5 · Turbulent Dispersion and the Gaussian Plume Model
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Environmental · L5 · Turbulent Dispersion and the Gaussian Plume ModelNote~437 words · 2 min
The Community Matrix Ecological network analysis formalizes a food web's dynamics near equilibrium with a community (Jacobian) matrix A, where a_ij captures how a small change in species j's abundance affects species i's per-capita growth r
Environmental · L5 · Ecological Network Analysis: May's Paradox and Real-World Food Web Structure
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Environmental · L5 · Ecological Network Analysis: May's Paradox and Real-World Food Web StructureNote~460 words · 2 min
Cohort vs Case-Control: The Core Design Trade-off Environmental epidemiology studies typically choose between two core designs. A cohort study follows exposed and unexposed groups forward in time, measuring exposure before disease onset — t
Environmental · L5 · Study Design and Causal Inference in Environmental Epidemiology
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Environmental · L5 · Study Design and Causal Inference in Environmental EpidemiologyNote~336 words · 2 min
Darcy's Law and the Flow Equation Groundwater flow modeling starts from Darcy's law — flow proportional to the hydraulic head gradient, scaled by hydraulic conductivity K: Extended to a full aquifer and combined with mass conservation, this
Environmental · L5 · Groundwater Flow and Contaminant Transport Modeling
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Environmental · L5 · Groundwater Flow and Contaminant Transport ModelingNote~476 words · 2 min
Three Sources of Climate Projection Uncertainty Climate projections carry uncertainty from three distinct sources, each behaving differently across the projection horizon. Because internal variability dominates near-term uncertainty while s
Environmental · L5 · Climate Model Uncertainty Quantification and Bayesian Calibration
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Environmental · L5 · Climate Model Uncertainty Quantification and Bayesian CalibrationPlot1 plot · 1 param
Atmospheric CO₂ Rise Since 1960 (Keeling Curve)
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Atmospheric CO₂ Rise Since 1960 (Keeling Curve)Plot1 plot · 1 param
Global Mean Sea-Level Rise Since 1900
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Global Mean Sea-Level Rise Since 1900Plot1 plot · 1 param
Radiative Forcing vs CO₂ Concentration
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Radiative Forcing vs CO₂ ConcentrationPlot1 plot · 1 param
Radioactive Decay: y = e^(−k·x)
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Radioactive Decay: y = e^(−k·x)Plot1 plot · 1 param
Temperature vs Altitude (Troposphere)
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Temperature vs Altitude (Troposphere)Plot1 plot · 1 param
Environmental · L5 · Radioactive Decay Curve: N(t) = N₀ exp(−λ t)
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Environmental · L5 · Radioactive Decay Curve: N(t) = N₀ exp(−λ t)Flowchart5 objects
Environmental · L1 · Air Pollution & Clean Air Quiz · flowchart
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Environmental · L1 · Air Pollution & Clean Air Quiz · flowchartFlowchart5 objects
Environmental · L1 · Earthquakes Quiz · flowchart
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Environmental · L1 · Earthquakes Quiz · flowchartFlowchart5 objects
Environmental · L4 · Solid Waste Management Engineering · flowchart
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Environmental · L4 · Solid Waste Management Engineering · flowchartFlowchart7 objects
Environmental · L1 · Farming & Growing Our Food Quiz · flowchart
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Environmental · L1 · Farming & Growing Our Food Quiz · flowchartFlowchart5 objects
Environmental · L1 · Deserts Quiz · flowchart
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Environmental · L1 · Deserts Quiz · flowchartFlowchart7 objects
Environmental · L1 · Air Pollution & Clean Air · flowchart
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Environmental · L1 · Air Pollution & Clean Air · flowchartFlowchart7 objects
Environmental · L1 · Earthquakes: Earth's Shaking Ground · flowchart
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Environmental · L1 · Earthquakes: Earth's Shaking Ground · flowchartFlowchart3 objects
Environmental · L3 · The Nitrogen Cycle · flowchart
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Environmental · L3 · The Nitrogen Cycle · flowchartFlowchart13 objects
Environmental · L3 · The Nitrogen Cycle · flowchart
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Environmental · L3 · The Nitrogen Cycle · flowchart