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Related Concept Videos

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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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.
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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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Variation of Atmospheric Pressure01:18

Variation of Atmospheric Pressure

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Change in atmospheric pressure with height is particularly interesting. The decrease in atmospheric pressure with increasing altitude is due to the decreasing gravitational force per unit area as we move away from the surface of the earth.
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
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The experimental conditions in a gravimetric analysis should be optimized to maximize the particle size and purity of the obtained precipitate. Ideally, the concentration of the precipitating reagent should be low with effective stirring to maintain low relative supersaturation for the growth of large crystals. In homogeneous precipitation, the precipitant is slowly generated by a chemical reaction in the solution to avoid local reagent excesses. For example, urea decomposes gradually to...
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Measurements of Waves in a Wind-wave Tank Under Steady and Time-varying Wind Forcing
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Evaluating and Extending the Ocean Wind Climate Data Record.

Frank J Wentz1, Lucrezia Ricciardulli1, Ernesto Rodriguez2

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|August 22, 2017
PubMed
Summary
This summary is machine-generated.

Satellite sensors have monitored ocean winds for 40 years, creating vital climate data records. Future continuity relies on intercalibrating new satellite data and addressing radiometer mission gaps.

Keywords:
Radar cross sectionremote sensingsatellite applicationssea surfacewind

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Area of Science:

  • Earth Science
  • Climate Science
  • Oceanography

Background:

  • Satellite microwave sensors (scatterometers and radiometers) have provided nearly 40 years of near-surface ocean wind data.
  • This data is crucial for studying and monitoring weather and climate variability.
  • Ocean Wind Climate Data Records (OW-CDRs) are developed by intercalibrating and merging various satellite wind datasets.

Purpose of the Study:

  • To ensure the continuity of ocean wind climate data records.
  • To evaluate and intercalibrate satellite-derived ocean wind measurements.
  • To address future challenges in maintaining long-term ocean wind monitoring.

Main Methods:

  • Intercalibration of satellite sensor measurements (e.g., OSCAT-2, QuikSCAT, RapidScat).
  • Comparison of satellite data with ocean buoys for validation.
  • Utilizing specialized model assimilations to create high-resolution wind vector grids.
  • Calibration of measurements using stable rainforest targets.

Main Results:

  • Established long-term ocean wind climate data records through sensor intercalibration and merging.
  • Identified challenges for future data continuity, including the failure of RapidScat and the lack of scheduled radiometer missions.
  • Demonstrated the utility of specialized model assimilations for compositing satellite wind information.

Conclusions:

  • Continued systematic monitoring of ocean winds is essential for climate studies.
  • Intercalibration and validation are critical for creating consistent and reliable climate data records.
  • Proactive planning is needed to address gaps in satellite observation systems for future climate monitoring.