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SCIENCE · INVESTIGATE AND EXPLAIN

Compare climate windows and trend summaries

Distinguish endpoint slopes from fitted slopes while retaining the full annual context.

Learning outcome: Calculate a per-decade endpoint change and explain how all-year fits and interval choices affect descriptive summaries.

Starting recap

Endpoint slopes use two observations; OLS uses all selected values. Observation count differs from elapsed years.

All lessons are open directly. Your saved experiments remain when you leave and return.

Try

For 1998–2012, endpoint slope is about 0.02857°C/decade but OLS slope is about 0.13393°C/decade.

Open the experiment

Predict

Must a line through the first and last values match a least-squares fit through the selected series?

Experiment

Compare 1959–2024, 1998–2012 and 2015–2024. Record coverage, counts and both slopes, retaining the full timeline.

Investigate recorded climate series

Recorded climate estimates · frozen historical series · Frozen climate-records-v1, selected through 2024. NASA GISTEMP v4 global land–ocean annual anomalies and NOAA/Scripps Mauna Loa annual dry-air CO₂ mole fractions are different observational products. Rebasing subtracts a constant. Descriptive ordinary least-squares trends are not causal attribution, forecasts or uncertainty intervals. No live data are requested.

Reset keeps your prediction, captures and practice history.

Snapshot climate-records-v1 retains annual temperature estimates for 1880–2024 and Mauna Loa CO₂ for 1959–2024. The complete bundled timeline remains visible; gold shading marks the selected interval. These are processed observational products, not direct readings from one global thermometer.

NASA GISTEMP v4 · global land–ocean temperature anomaly (°C)Source baseline: 1951–1980 · dashed line: selected least-squares fit-1.5-1-0.500.511.518801920196020002024Year · full context retained for every selection
NOAA / Scripps Mauna Loa record · CO₂ mole fraction (ppm)Different quantity and spatial coverage · not a global temperature record300320340360380400420440Before 1959:unavailable18801920196020002024Year · same time axis, separate physical units
Descriptive statistics for available annual values in the selected interval
QuantityTemperature anomaly (°C)CO₂ mole fraction (ppm)
Actual coverage1959–20241959–2024
Available / unavailable years66 / 066 / 0
Arithmetic mean of available annual values0.3868360.2495
Least-squares slope per decade0.176816.5669
First-to-last slope per decade0.192316.7123
Subtracted temperature baseline offset0.000000 °CNot applied to CO₂

The fit uses every available annual value in the interval with equal weight: slope per decade = 10 × Σ[(year − mean year)(value − mean value)] / Σ[(year − mean year)²]. The endpoint slope uses only the first and last available values. Neither describes every year's change. No confidence interval or significance test is calculated; annual climate values are not assumed to be independent random samples.

Inspect all selected annual source values
Frozen annual estimates, with source and rebased anomalies kept separate
YearSource anomaly °C (1951–1980)Selected anomaly °CCO₂ ppmReported CO₂ uncertainty ppm
19590.030.0300315.980.12
1960-0.02-0.0200316.910.12
19610.060.0600317.640.12
19620.030.0300318.450.12
19630.050.0500318.990.12
1964-0.20-0.2000319.620.12
1965-0.11-0.1100320.040.12
1966-0.06-0.0600321.370.12
1967-0.02-0.0200322.180.12
1968-0.08-0.0800323.050.12
19690.050.0500324.620.12
19700.030.0300325.680.12
1971-0.08-0.0800326.320.12
19720.010.0100327.460.12
19730.160.1600329.680.12
1974-0.07-0.0700330.190.12
1975-0.01-0.0100331.130.12
1976-0.10-0.1000332.030.12
19770.180.1800333.840.12
19780.070.0700335.410.12
19790.160.1600336.840.12
19800.260.2600338.760.12
19810.320.3200340.120.12
19820.140.1400341.480.12
19830.310.3100343.150.12
19840.160.1600344.870.12
19850.120.1200346.350.12
19860.180.1800347.610.12
19870.320.3200349.310.12
19880.390.3900351.690.12
19890.270.2700353.200.12
19900.450.4500354.450.12
19910.410.4100355.700.12
19920.220.2200356.540.12
19930.230.2300357.210.12
19940.310.3100358.960.12
19950.450.4500360.970.12
19960.330.3300362.740.12
19970.470.4700363.880.12
19980.610.6100366.840.12
19990.380.3800368.540.12
20000.390.3900369.710.12
20010.530.5300371.320.12
20020.630.6300373.450.12
20030.620.6200375.980.12
20040.530.5300377.700.12
20050.680.6800379.980.12
20060.640.6400382.090.12
20070.660.6600384.020.12
20080.540.5400385.830.12
20090.660.6600387.640.12
20100.720.7200390.100.12
20110.610.6100391.850.12
20120.650.6500394.060.12
20130.670.6700396.740.12
20140.750.7500398.810.12
20150.890.8900401.010.12
20161.011.0100404.410.12
20170.910.9100406.760.12
20180.850.8500408.720.12
20190.980.9800411.650.12
20201.011.0100414.210.12
20210.850.8500416.410.12
20220.890.8900418.530.12
20231.171.1700421.080.12
20241.281.2800424.610.12

NOAA defines the annual uncertainty column from the standard deviation of differences between independently determined NOAA and Scripps annual means; it is not a regression confidence interval. The source temperature table supplies no annual uncertainty column here. Decimal precision does not imply zero uncertainty. Temperature rebasing uses the mean of 30 rounded annual anomalies; the native 1951–1980 annual mean can differ slightly from zero because of rounding.

Mauna Loa is a background-air observing location, not a global mean or emissions inventory. Its record includes Maunakea observations during the 2022–2023 eruption interruption. The bundled analysis stops at 2024 to use a fixed historical window; it is not a claim about the latest year. Upstream revisions do not silently replace this snapshot.

Sources: NASA GISTEMP v4, Lenssen and colleagues (2024), observational uncertainty, and NOAA / Scripps CO₂ data. Retrieved 25 October 2026. Two rising series alone do not establish causal attribution; physical mechanisms, alternative drivers and independent evidence are also needed. There is no CO₂-to-emissivity calibration or forecast in this investigation.

Temperature trend 0.1768 °C per decade across 66 annual estimates; CO₂ trend 16.5669 ppm per decade across 66 available annual means.

Selected interval 1959–2024. Temperature reference shift 0.000000 °C. CO₂ coverage 1959–2024; 0 years unavailable in this selection. Missing values are not zero. Co-trends alone do not identify a cause.

Captures preserve interval and reference-period selections in climate-records-v1 and replay descriptive calculations from frozen NASA and NOAA/Scripps annual products. They are not new measurements, live updates or causal experiments.

Understand

Ask what a slope summarizes

A climate record can fluctuate from year to year while changing over a longer interval. This lab offers several explicit analysis windows and keeps the full record visible. The window changes which observations enter a summary; it does not erase years outside the selection.

Begin with 1959–2024 and the native temperature reference. Write down the number of annual values, the mean, the endpoint slope and the fitted slope. Before switching to 1998–2012, predict whether the two slope methods must agree. They summarize the same selected series in different ways, so agreement is not guaranteed.

These are real annual estimates from a frozen NASA GISTEMP dataset. They are not a controlled experiment in which only one climate influence changes. Short-term departures from a fitted line should be described before any explanation for them is assigned.

Calculate an endpoint slope carefully

The endpoint slope uses only the first and last values. In the stored data, 1998 is +0.61°C and 2012 is +0.65°C relative to 1951–1980. Their difference is +0.04°C over 2012 − 1998 = 14 elapsed years.

Divide 0.04 by 14 and multiply by ten to express the result per decade: about +0.02857°C/decade. There are fifteen annual observations when both endpoints are included, but only fourteen years between them. Confusing count with elapsed time changes the denominator.

On paper, draw the two endpoints and connect them. Then add a few interior values from the selected record. The connecting line did not use those interior observations. That omission is a property of the method, not evidence that the interior values are unimportant.

Fit a line using all selected years

Ordinary least squares, or OLS, chooses an intercept and slope that minimize the sum of squared vertical residuals between the line and the data. A residual is an observed anomaly minus the fitted value for that year. Squaring prevents positive and negative residuals from cancelling in the objective.

For 1998–2012, the fitted slope is about +0.13393°C/decade, substantially different from the endpoint result. The interior observations affect the fitted line. For 1959–2024 the temperature OLS slope is about +0.17679°C/decade in this snapshot.

The fitted slope is a descriptive linear summary of its selected interval. It does not mean every year increases by that amount, that the underlying response is exactly linear, or that the same slope predicts all future years. Nor does choosing OLS make the selected period automatically representative of every climate question.

Compare windows without hiding the choice

Use 1981–2024, 1998–2012 and 2015–2024. For each, record actual coverage, count and both slopes. Explain differences with reference to the visible values and interval length before offering a physical interpretation. Keep the full timeline beside your table so a short-window claim cannot quietly replace a long-record conclusion.

Change the anomaly reference while holding one window fixed. The fitted and endpoint slopes remain unchanged because a constant vertical shift changes neither differences nor the best-fitting slope. If your hand calculation changes, inspect inconsistent baselines or rounding.

Source uncertainty and trend uncertainty are distinct. The lab’s slope is not accompanied by a regression confidence interval, and a source uncertainty for another variable cannot serve as one. Temperature observations also need not be independent annual draws. NASA’s uncertainty research treats observational uncertainty beyond this descriptive exercise.

Transfer with a short constructed series

A paper series at years 0, 1, 2, 3 and 4 has values 0, 0, 0, 4 and 0. Its endpoint slope is zero. Does that force its OLS slope to be zero? Explain what additional information the fitted line uses.

Check the climate-windows transfer

No. The interior value of 4 at year 3 shifts the fitted slope positive; using mean year 2, the slope is 4/10 = 0.4 units per year. The endpoint method misses that interior structure. Neither summary alone identifies a physical cause.

Apply

The elapsed time between annual values labeled 1998 and 2012 is:

Public practice checks a specific claim. It does not establish independent mastery.

Explain method and window dependence without assigning a physical cause from the fitted line alone.

Continue

Completion requires a saved prediction, at least one capture and a reflection. Presence checks do not grade your reasoning.

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