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Thermometers and Temperature Scales01:22

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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.
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Temperature-Dependent Growth of Brook TroutThe growth of brook trout is closely influenced by water temperature. Experimental data demonstrate how trout weight changes over a 24-day period in response to varying water temperatures. At lower temperatures, such as 15.5 degrees Celsius, brook trout show significant weight gain. However, as the temperature increases, the amount of weight gained steadily decreases. At the highest temperature measured, 24.4 degrees Celsius, trout experience a net...
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Freshwater systems such as streams, rivers, and lakes exhibit distinct physical and biological characteristics that influence their microbial communities. These environments are broadly categorized into lotic systems—those with flowing waters like streams and most rivers—and lentic systems, which include still or slow-moving waters such as lakes, ponds, and marshes.In lentic systems, phytoplankton drive primary production, generating autochthonous organic carbon. In contrast, lotic...
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The expansion of alcohol in a thermometer is one of many commonly encountered examples of thermal expansion, which is the change in size or volume of a given system as its temperature changes. The most visible example is the expansion of hot air. When air is heated, it expands and becomes less dense than the surrounding air, which then exerts an upward force on the hot air to, for example, make steam and smoke rise, and hot air balloons float. The same behavior happens in all liquids and gases,...
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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.
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The body's temperature, measured in degrees, is determined by the balance between heat production and dissipation to the surrounding environment. For instance, if exercising vigorously, the body will produce more heat, causing sweat and dissipating that heat. Despite extreme environmental conditions and physical exertion, the human temperature-control system maintains a constant core body temperature (the temperature of deep tissues, which are the tissues located beneath the skin and other...
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Diel Surface Temperature Range Scales with Lake Size.

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Small lakes experience significant daily temperature swings, impacting aquatic ecosystems. These diel temperature ranges are substantial in summer and increase with smaller lake size.

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Area of Science:

  • Environmental Science
  • Limnology
  • Climate Science

Background:

  • Lake ecological and biogeochemical processes are temperature-dependent.
  • Long-term lake surface warming is documented, but diel (daily) temperature variations are less understood due to data limitations.

Purpose of the Study:

  • To quantify the pattern and magnitude of diel surface water temperature variability.
  • To investigate the relationship between lake size and diel temperature fluctuations.

Main Methods:

  • Utilized high-frequency temperature data from 100 lakes.
  • Analyzed near-surface water temperature patterns across diel timescales.

Main Results:

  • Diel temperature ranges in summer can be substantial compared to long-term warming trends.
  • For lakes smaller than 3 km², diel temperature range increases sharply with decreasing lake area.
  • Most small lakes studied showed average summer diel ranges of 4–7°C.

Conclusions:

  • Significant diel temperature fluctuations in most lakes impact aquatic ecosystem structure and function.
  • The full implications of large diel temperature variations on lake biogeochemical cycles require further exploration.