HSC Geography · Teaching presentation

13.1 Characteristics of Climate Change

Spatial & temporal · reading the climate data · Chapter 13
Laptops down · copy the ✍️ notebook boxes as we go

What we're doing today ✍️ Copy into your notebook

Chapter 13 examines climate change in depth. This first lesson tackles the foundational question: what does the data actually show? Not why it is happening (that's 13.2) or what it does (13.3), but the observed pattern itself — where (spatial) and when (temporal) the planet is warming. Getting these two dimensions straight is the backbone of every response you'll write on climate change, because markers want the pattern described precisely and quantified with real figures — not just “it's getting hotter.”

By the end you can:

  • state the scientific consensus;
  • describe the warming trend over time;
  • explain ocean warming & storms;
  • describe the spatial pattern (Arctic fastest);
  • quote Australian evidence.
Fossil-fuel emissions drive the trend
Extreme heat — a felt consequence

Consensus & definitions ✍️ Copy into your notebook

Weather vs climate — weather = the day-to-day state of the atmosphere; climate = the long-term average pattern, measured over 30+ years.

Climate scientists overwhelmingly agree that Earth is warming and that human activity is the main cause: repeated surveys of the peer-reviewed literature put the consensus at over 97% of actively publishing climate scientists. Australia's own authorities — the Bureau of Meteorology and CSIRO, in their biennial State of the Climate report — reach the same conclusion. The scientific question is settled; the political and public argument about what to do about it is a separate thing. Don't confuse the two in an exam.

Don't confuse settled science with ongoing politics.
A warming world = more energetic weather
The signal is clear in the ice
📘 Syllabus: Human–Environment Interactions · climate change🧭 Skill: Evidence vs opinion
Temporal

The warming over time

The global data ✍️ Copy into your notebook

baseline (late-19th-C) 0+0.5+1.0 18501950now >+1.1°C

The headline figure: about 1.1–1.2 °C of warming since the late 1800s, and the pace has accelerated — most of it has come in the last ~40 years. The graph plots the temperature anomaly — the difference from a late-19th-century baseline, not the absolute temperature. The record is maintained by NASA's GISTEMP and confirmed independently by other teams.

The warming, in numbers
  • ~1.1–1.2°C warmer than the late-1800s baseline.
  • The 10 warmest years on record are all since 2010.
  • Current warming rate ~0.2°C per decade.
  • A temperature anomaly = difference from a baseline, not absolute °C.
  • Pre-industrial baseline: the 1850–1900 average.
📘 Syllabus: Human–Environment Interactions · climate change🧭 Skill: Reading an anomaly graph

Why we trust the trend ✍️ Copy into your notebook

Reliability comes from independent agreement. At least five separate teams process the raw temperature records using their own methods — different corrections, different handling of gaps — and every one of them reaches the same trend. That convergence is itself powerful evidence: a mistake in one method would show up as disagreement, not as five graphs that lie almost on top of each other. You can rebuild the global series yourself from NOAA's Climate at a Glance tool.

Independent datasets agreeing rules out any single method's error.
The datasets
  • NASA GISTEMP (USA).
  • NOAA NCEI (USA).
  • HadCRUT — UK Met Office & Hadley Centre.
  • Berkeley Earth (independent, USA).
  • ECMWF ERA5 reanalysis (Europe).
📘 Syllabus: Human–Environment Interactions · climate change🧭 Skill: Data reliability
The oceans

Ocean warming

Sea-surface temperature ✍️ Copy into your notebook

20th-C average 18801950now SST anomaly

The ocean is the planet's great heat store, absorbing more than 90% of the extra energy that greenhouse gases trap. That's why sea-surface temperature has climbed steadily since 1880, tracked in NOAA's ocean records. Warmer surface water is the fuel for storms: it feeds more energy into tropical cyclones, hurricanes and typhoons, making them more intense — heavier rain, stronger winds — even if they don't grow more frequent.

Ocean heat, in numbers
  • Oceans absorb >90% of the Earth's excess heat.
  • Global SST up ~0.9°C since pre-industrial (IPCC AR6).
  • Marine heatwaves have roughly doubled since the 1980s.
  • Warm water = storm fuel → more intense cyclones.
  • Storm intensity rises; frequency need not.
📘 Syllabus: Human–Environment Interactions · climate change🧭 Skill: Cause & consequence
Spatial

Where the warming is

Global but uneven ✍️ Copy into your notebook

Arctic — warming fastest Almost everywhere warmer than average deeper red = greater warming

Anomaly maps — like those from NASA — show the warming is near-global: almost every region is warmer than its 20th-century average, and vanishingly few areas have cooled. But it is uneven. Land warms faster than ocean, and the Arctic warms fastest of all — roughly three to four times the global rate (“Arctic amplification”, from 12.1), as reflective sea ice melts and exposes dark, heat-absorbing water.

The spatial pattern
  • Near-global: almost every region warmer than average.
  • Land warms faster than ocean.
  • The Arctic warms ~3–4× the global rate.
  • Driver: the ice–albedo feedback (less ice = more heat absorbed).
  • Very few regions on Earth have cooled at all.
📘 Syllabus: Human–Environment Interactions · climate change🧭 Skill: Interpreting a thematic map
At home

Climate change in Australia

The Australian record (BoM) ✍️ Copy into your notebook

+0.15–0.2°Cwarming per decade2019warmest year (then)wholecontinent warmed

Australia has warmed about 1.5 °C since national records began in 1910 — faster than the global average — according to the Bureau of Meteorology and CSIRO. The trend is both temporal (a clear rise) and spatial (virtually the whole continent), and it brings more dangerous fire weather (→ Chapter 14).

Temporal (a clear trend) AND spatial (everywhere) — and more fire weather.
What the record shows
  • Reliable data since 1910 (BoM).
  • ~1.5°C of warming since 1910.
  • ~0.15–0.2 °C warming per decade since 1970.
  • Virtually the whole continent has warmed.
  • Dangerous fire-weather days up sharply.
📘 Syllabus: Human–Environment Interactions · climate change🧭 Skill: Sourcing verified data

Watch: the warming, visualised ✍️ Copy into your notebook

Numbers on a page can feel abstract. This short NASA visualisation animates the global temperature record from 1880 to 2022, painting each year's anomaly onto a world map. Watch the colours shift from blue (cooler than average) to deep red — and notice how the reddening speeds up, and where it bites hardest.

▶ Watch: Global Warming from 1880 to 2022 — ARCHIVED - NASA Climate Change (click → opens on YouTube)

As you watch, note: (1) roughly which decade the map tips from mostly blue to mostly red; (2) which region reddens fastest and deepest; (3) how the animation shows a temporal and a spatial pattern at the same time.

📘 Syllabus: Human–Environment Interactions · climate change🧭 Skill: Interpreting a data visualisation

Sources & explore further ✍️ Copy into your notebook

Every figure in this lesson comes from a primary dataset — an official temperature record you can open and read yourself. Being able to name and cite the source of your data is exactly what separates a Band 5–6 response from a Band 3–4 one. Bookmark these for your research task.

Dataset — a compiled, quality-controlled record (e.g. NASA GISTEMP) that scientists use to track climate over time. Cite it by name, not a random blog.
📘 Syllabus: Human–Environment Interactions · climate change🧭 Skill: Referencing sources

Practise the skill ✍️ Copy into your notebook

“Describe the spatial and temporal characteristics of recent climate change, using evidence.”
Temporal — ~1.1 °C since 1880; fastest recently; datasets agree.
Spatial — near-global; Arctic fastest; whole of Australia.
Evidence — name a dataset (NASA/BoM) and a figure.
Link — oceans warming → more intense storms.
Marks come from
  • Naming both spatial AND temporal.
  • Using a specific figure (°C, year).
  • Citing a source (NASA, NOAA, BoM).
  • Correct use of “anomaly.”
📘 Syllabus: Human–Environment Interactions · climate change🧭 Skill: Short response

Glossary recap ✍️ Copy into your notebook

Climate — the long-term average pattern of weather (30+ years).
Temperature anomaly — the difference from a long-term average — not the absolute temperature.
Sea-surface temperature — the temperature of the top ~1 mm of the ocean; fuels storms.
Temporal characteristic — how something changes over time.
Spatial characteristic — how something varies across place.
Scientific consensus — the settled agreement among peer-reviewed scientists.
Dataset — a compiled record (e.g. NASA GISTEMP) used to track climate.
Arctic amplification — the Arctic warming far faster than the global average (ice–albedo feedback).
Fire weather — hot, dry, windy conditions that raise bushfire danger — increasing in Australia.
Next lesson

13.2 — Causes of climate change

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