The degree to which a measurement or computation result matches the true or intended value.Accuracy is the degree to which a measurement or calculation matches the true or intended value. It is distinct from precision, which describes how reproducible a measurement is. A measurement can be precise but inaccurate if a systematic error shifts all results away from the truth. In physics, accuracy is essential for validating theories and for engineering applications where exactness matters.
The concept of accuracy has been implicit in measurement since antiquity, but it was formalized in the 19th century with the development of error analysis by mathematicians like Carl Friedrich Gauss. The distinction between accuracy and precision became standard in the 20th century with the rise of experimental physics.
Accuracy is assessed by comparing a measured value to a known standard or reference. For example, a ruler might be accurate to within 0.5 millimeters, meaning any measurement could deviate from the true length by at most that amount. Systematic errors — such as a miscalibrated instrument or a biased experimental setup — reduce accuracy, while random errors affect precision. Improving accuracy often involves calibration against standards, correcting for known biases, and using more refined measurement techniques.
Accuracy is critical in GPS navigation, where meter-level errors can cause significant positional mistakes, and in metrology, where national standards laboratories maintain ultra-accurate references for units like the meter and the second.
The most accurate measurement ever made is the speed of light in a vacuum, which is defined as exactly 299,792,458 meters per second — so accurate that it now defines the meter itself.
