The recent declaration that 2023 marked the hottest year in recorded history came with a surprising revelation: uncertainty about the exact degree of global warming. Divergent findings by climate scientists present a discrepancy, with one group indicating a 1.34°C increase over the 1850–1900 baseline and another suggesting a 1.54°C rise. The crux of the disagreement lies not in present temperatures but in historical data, particularly the late 19th-century oceanic warmth used as a benchmark for assessing planetary warming.

Challenges in Historical Temperature Records:

  1. Oceanic Temperature Records:

    • Ocean temperature records from the 19th century are scarce.
    • Matthew Fontaine Maury initiated global records in the 1850s, encouraging sailors to collect weather observations, including water temperature, in exchange for naval charts.
  2. Methodological Biases:

    • Evolving measurement methods, from wooden buckets to sensors along ship hulls, introduced biases.
    • The U.S. National Oceanic and Atmospheric Administration (NOAA) and the U.K.’s Met Office maintain historical sea surface temperature records, employing different correction methodologies.

Methodological Approaches:

  1. NOAA's Cross-Checking:

    • Cross-checks bucket temperatures with contemporaneous air temperatures.
    • Suggests less ocean warming over the past 170 years compared to the Met Office.
  2. Met Office's "Bucket Model":

    • Utilizes a model to estimate water temperature before being collected in a bucket.
    • Assumes certain bucket types if not documented.

Addressing Bias and Discrepancies:

  1. Temperature Adjustments:

    • Duo Chan proposes using nearby island or coastal weather stations to adjust shipboard observations for bucket biases.
    • Corrects artifacts like late 1800s cooling and rapid warming from 1910 to World War II.
  2. Detailed Analysis:

    • Elizabeth Kent and colleagues scrutinize logbooks for overlooked details to infer data collection methods.
    • Grouping ships by country reveals measurement differences, such as the post-1930s temperature drop in Japanese records due to digitization.

The Path Forward:

  1. Digitization Challenges:

    • A substantial number of logbooks remain untouched, presenting an untapped source of data.
    • Ed Hawkins highlights the need for accelerated digitization efforts using machine reading and artificial intelligence.
  2. Importance of Data Refinement:

    • Beyond clarifying current global warming rates, refined historical records offer insights into regional variations in ocean warming.
    • Enhances models' accuracy in predicting future global warming trends.

As efforts intensify to reconcile historical temperature discrepancies, the quest for precision in assessing the pace of global warming and refining climate models remains paramount. The complex tapestry of historical ship logs holds the key to unlocking a more accurate understanding of Earth's warming journey.

More: https://www.science.org/content/article/world-1-3%C2%B0c-or-1-5%C2%B0c-warmer-historical-ship-logs-hold-answers