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Global Climate Change01:50

Global Climate Change

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Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
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Temperature Measurement Sites01:14

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A thermometer measures body temperature. The common sites for measuring body temperature are the oral cavity, axillary region, temporal artery, and skin surface, such as the forehead, abdomen, and axilla. True core body temperature is assessed in the rectum, tympanic membrane, pulmonary artery, esophagus, and urinary bladder.
Oral: When assessing oral temperature, the thermometer tip should be placed under the tongue in the posterior sublingual pocket. It offers accurate readings and can be...
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Assessing Body Temperature - Temporal Artery01:19

Assessing Body Temperature - Temporal Artery

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Here is a stepwise guide to assessing the body temperature at the temporal artery using a temporal artery thermometer
Step 1: Perform hand hygiene and don a fresh pair of gloves to prevent cross-infection and ensure patient safety.
Step 2: Explain the procedure to the patient to establish trust. Clear communication establishes trust with the patient, ensures they understand what to expect, promotes cooperation, and enhances comfort during the procedure.  
Step 3: Assess the patient's...
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What is Climate?01:16

What is Climate?

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Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
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Thermometers and Temperature Scales01:22

Thermometers and Temperature Scales

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Any physical property that depends consistently and reproducibly on temperature can be used as the basis of a thermometer. For example, volume increases with temperature for most substances. This property is the basis for the common alcohol thermometer and the original mercury thermometers. Other properties used to measure temperature include electrical resistance, color, and the emission of infrared radiation.
As many physical properties depend on temperature, the variety of thermometers is...
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Precipitation Gravimetry01:03

Precipitation Gravimetry

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Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
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Updated: Apr 12, 2026

Removal of Exogenous Materials from the Outer Portion of Frozen Cores to Investigate the Ancient Biological Communities Harbored Inside
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An extended Arctic proxy temperature database for the past 2,000 years.

Nicholas P McKay1, Darrell S Kaufman1

  • 1School of Earth Sciences and Environmental Sustainability, Northern Arizona University , Flagstaff, Arizona 86011, USA.

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|May 16, 2015
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Summary

This study revises an Arctic temperature database (version 1.1) for the past 2,000 years. The enhanced dataset aids in understanding modern warming within natural climate variability.

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Area of Science:

  • Paleoclimatology
  • Climate Science
  • Arctic Research

Background:

  • Robust climate reconstructions are essential for contextualizing current warming trends against natural climate variability.
  • Previous reconstructions of Arctic temperatures have relied on proxy data, necessitating improvements in data quality and uncertainty assessment.

Purpose of the Study:

  • To present an extended and revised database (version 1.1) of proxy temperature records for the Arctic over the past 2,000 years.
  • To provide datasets in a machine-readable format with enhanced geochronologic data and time-uncertainty ensembles for future analyses.
  • To include standardized seasonality information for each proxy record to facilitate nuanced integration.

Main Methods:

  • Revision and extension of an existing database of proxy temperature records.
  • Inclusion of geochronologic data and generation of time-uncertain ensembles.
  • Standardization of seasonality descriptions for each proxy record.

Main Results:

  • The revised database (version 1.1) offers improved data quality and uncertainty quantification for Arctic temperature reconstructions.
  • Despite a predominance of seasonal temperature responders, the database effectively captures annual temperature variability across the Arctic.
  • The highest density of records, particularly in northeast Canada and Greenland, shows the strongest correlation with annual temperature variability.

Conclusions:

  • The enhanced Arctic temperature database provides a valuable resource for understanding long-term climate change and natural variability.
  • The inclusion of geochronologic uncertainty and seasonality information enables more sophisticated paleoclimate analyses.
  • The database confirms its utility in reconstructing past Arctic temperatures, especially in data-rich regions.