ENVIRONMENTAL GIS · WATER QUALITY · SPATIAL INTERPOLATION

Mapping dissolved oxygen across Chesapeake Bay.2015 · 2025 comparison

I used supplied monitoring observations to build dissolved-oxygen surfaces for 2015 and 2025 and display them on the same scale.

Data preparationSpatial interpolationRaster comparisonCartography

01 / SPATIAL COMPARISON

The 2015 and 2025 surfaces use the same scale

Lower dissolved-oxygen estimates appear in warm colors and higher estimates in green across a shared 3–9 mg/L display range.

Side-by-side maps of interpolated dissolved oxygen levels in Chesapeake Bay for 2015 and 2025, using a common red-to-green scale from 3 to 9 milligrams per liter.
Interpolated dissolved-oxygen surfaces · Chesapeake Bay · 2015 and 2025

02 / ANALYTICAL WORK

How I built the two surfaces

The observations were supplied to me; my work began with preparing them for analysis and continued through interpolation, comparison, and map design.

  1. 01

    Prepare the supplied data

    Organize the provided dissolved-oxygen observations for consistent spatial processing and year-to-year comparison.

  2. 02

    Interpolate continuous surfaces

    Transform discrete observations into estimated dissolved-oxygen surfaces covering the sampled portions of Chesapeake Bay.

  3. 03

    Standardize the comparison

    Use a common geographic extent, measurement unit, and color scale so differences between 2015 and 2025 can be read consistently.

  4. 04

    Design the final map

    Combine the analytical surfaces with reference geography, labels, legend, scale, orientation, and source information.

03 / INTERPRETATION

What interpolation can and cannot tell us

Spatial interpolation estimates conditions between monitoring locations. It does not turn every mapped pixel into a direct field measurement.

What the map supports

Visual comparison of broad spatial patterns in the supplied 2015 and 2025 dissolved-oxygen observations.

What affects interpretation

Sampling location, water depth, season, temperature, salinity, and station density can influence dissolved-oxygen patterns and the interpolated result.

What it does not establish

Two mapped periods alone do not demonstrate a causal environmental trend or conditions at every location in the Bay.

04 / TEACHING APPLICATION

A practical way to teach interpolation and uncertainty

I would use this comparison to show how point observations become a continuous surface, how station spacing affects the result, and why an interpolated pixel is an estimate rather than a direct measurement.

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