University of Melbourne · S1 2026 · FACULTY OF ENVIRONMENTAL SCIENCE

EVSC10001 · The Global Environment

- one subject, every graph, every model, every mark
50% final exam · hurdle8 Chapters80-page Bible
Our own words - no uploaded lecturer files
Built to mirror S1 2026 · updated this semester
The Complete Exam Bible · S1 2026

The Global Environment

— one subject, every system, every diagram, every mark

The Global Environment treats Earth as a set of interacting systems — from the origin of the planet and rocks, through plate tectonics, the history of life, and deep-time climate, to the modern atmosphere, oceans, the greenhouse effect and the surface processes that shape landscapes. The final exam is 60% of your grade, closed-book and a hurdle, and every short-answer requires a labelled diagram — so this guide teaches each system as a diagram you can draw and annotate from memory.

EVSC10001 · University of Melbourne
Assessment

How EVSC10001 is assessed

ComponentWeightFormat
Final exam · hurdle60%Closed-book, 2 hours · Part A short-answer (70%, answer 7 of 9, a labelled diagram required for each) + Part B 30 multiple-choice (30%) · hurdle
Weekly practical quizzes · hurdle20%Ten in-class LMS quizzes across the semester · hurdle
Group research poster · hurdle20%Jointly produced poster (~1000-word equivalent), due before mid-semester · hurdle
Worked example · free

The greenhouse energy balance — the diagram examiners want, mark by mark

Q [6 marks]. Explain the greenhouse effect using an energy-balance diagram. Show why adding greenhouse gases warms the surface.
  • +1Draw incoming shortwave solar radiation; show part reflected by clouds/surface (albedo) and part absorbed at the surface.
  • +1Show the warmed surface emitting longwave (infrared) radiation upward.
  • +2Draw greenhouse gases (CO₂, H₂O, CH₄) absorbing and re-emitting that infrared in all directions, including back down (back-radiation).
  • +1State the balance: at steady state, energy in = energy out; back-radiation raises the surface temperature above the no-atmosphere value.
  • +1Conclude: more greenhouse gas ⇒ more infrared absorbed and re-radiated downward ⇒ a warmer surface (enhanced greenhouse effect).
Solar shortwave is absorbed at the surface; the surface re-emits infrared; greenhouse gases absorb and re-radiate it downward; adding gas increases back-radiation and warms the surface.
Sia tip — In Part A the labelled diagram earns the marks — arrows with the radiation type and direction score more than prose. Always label shortwave in, infrared out, and the back-radiation arrow.
Glossary

Key terms

Plate tectonics
The theory that Earth's rigid lithosphere is broken into plates that move over the asthenosphere, interacting at divergent, convergent and transform boundaries — the engine of earthquakes, volcanoes and mountain building.
The rock cycle
The continuous transformation among igneous, sedimentary and metamorphic rocks through melting, weathering and erosion, deposition and lithification, and heat and pressure.
Milankovitch cycles
Cyclic variations in Earth's orbit — eccentricity, obliquity (tilt) and precession — that change the seasonal and latitudinal distribution of sunlight and pace the glacial–interglacial cycles.
The greenhouse effect
Warming of the surface because greenhouse gases absorb outgoing infrared radiation and re-emit it, including back toward the surface; the enhanced effect is the added warming from extra gases.
Thermohaline circulation
The global deep-ocean 'conveyor' driven by differences in temperature and salinity (hence density), redistributing heat between low and high latitudes.
Weathering
The in-place breakdown of rock by physical processes (e.g. freeze–thaw) and chemical reactions (e.g. dissolution, hydrolysis); the precursor to soil formation and erosion.
FAQ

EVSC10001 FAQ

Is EVSC10001 hard?

It is broad rather than mathematically hard: the challenge is connecting many Earth systems and being able to draw and label the key diagrams from memory. Because the exam is 60%, closed-book and a hurdle, and every short-answer needs a labelled diagram, diagram fluency is the difference.

How is EVSC10001 assessed?

A 60% closed-book final exam (a hurdle), 20% weekly practical quizzes (a hurdle) and a 20% group research poster (a hurdle). You must pass the exam and the practical work to pass the subject. Confirm details in your subject guide.

What's on the EVSC10001 exam?

Two hours: Part A is short-answer (answer 7 of 9 topics, each needing a labelled diagram, worth 70%) and Part B is 30 multiple-choice (30%). It spans the whole subject — origins and rocks, plate tectonics, life and extinctions, deep-time and modern climate, atmosphere/ocean, weathering/soils and surface landforms.

Why does every answer need a diagram?

The exam explicitly requires a labelled diagram or sketch for each Part-A answer, so the marks reward a clear, correctly annotated figure as much as the explanation. Practise drawing each core system (rock cycle, plate boundaries, greenhouse balance, circulation cells) from a blank page.

Is using AskSia for EVSC10001 cheating?

No. AskSia is a study reference written in our own words — we host none of your lecturer's files, and Sia teaches you the method to earn the marks; it does not complete or sit your assessments.

Study strategy

How to study for the exam

Make the diagrams your study unit. For every system — the rock cycle, the three plate boundaries, the geological timescale, Milankovitch forcing, the atmospheric circulation cells, the thermohaline conveyor, the greenhouse energy balance, soil horizons and the river/glacier/coast landforms — practise drawing and fully labelling it from a blank page, because Part A awards the labelled diagram directly. Then attach a two-sentence mechanism to each. Master nine systems well and you can always answer 7 of 9.

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