The information listed below was provided by the National Oceanic and Atmospheric Administration's Hurricane Research division.
Subject: F8) How is storm surge observed and measured?
Contributed by the NHC Storm Surge Unit
There are several methods used by NOAA, the United States Geological Survey (USGS), and the Federal Emergency Management Agency (FEMA) to measure storm surge. Each method has advantages and draw backs and post-storm analysis of storm surge requires resolving differences in what each measures to find the best approximation of the surge heights.
A network of 175 long-term, continuously operating water level stations located throughout the U.S. serving as the foundation for NOAA's tide prediction products.
These are the lines left on trees and structures marking the highest (peak) elevation of the water surface from a flood event. They are created by foam, seeds, and other debris. Survey crews deploy after a storm, locate, and record reliable high water marks. GPS methods are used to determine the location of these marks, which are then mapped relative to a vertical reference datum.
These are temporary water-level and barometric-pressure sensors which provide information about storm surge duration, times of surge arrival and retreat, and maximum depths.
The three main routes for taking a temperature are oral, rectal, and axillary (underarm). Oral measurements are taken in the mouth, rectal measurements are taken in the rectum, and axillary measurements are taken in the armpit. Each route can provide slightly different readings, so it's important to use the same method consistently for accurate comparisons.
A tropical storm watch means that tropical storm conditions, including strong winds and heavy rain, are possible within the specified area within the next 48 hours. It is a warning for residents to start taking precautions and preparing for the potential impacts of the approaching storm.
Yes, by taking multiple measurements and calculating the average, you can reduce the impact of random errors and get closer to the actual density. This is because averaging multiple measurements helps to minimize the effects of outliers or individual errors in any single measurement.
You can get to Daintree Rainforest by flying to Cairns in Australia, and then either renting a car to drive north for about 2 hours or taking a guided tour. The rainforest is located in Tropical North Queensland.
Tide measurements are typically taken at a tidal station or tide gauge located along the coastline or in coastal waters. These stations are equipped with sensors to measure water levels and provide data on tidal patterns.
SATELLITE
Yes, satellites are the main instrument for taking measurements of tropical cyclones far out at sea. Satellites can provide valuable data on the cyclone's intensity, size, and movement, which is crucial for forecasting its trajectory and potential impact on land. This information is used by meteorologists to issue warnings and advisories to help protect people and property in the path of the cyclone.
A theodolite is an instrument that is used in archaeoastronomy. To change the face for taking angle measurements when using a theodolite you must turn the telescope by 180 degrees.
A negative sight in surveying occurs when the vertical line of sight from the instrument to the target is below the instrument's horizontal axis. This can result in incorrect measurements and lead to inaccuracies in the survey data. Negative sights should be avoided by ensuring that the instrument is properly leveled before taking measurements.
Making careful sketches and Taking careful measurements
Zero error of an instrument refers to a condition where the instrument does not read zero when it should. This can occur due to miscalibration, physical damage, or wear and tear, leading to inaccurate measurements. It can result in systematic errors in readings, affecting the reliability of the data collected. To ensure precision, it’s essential to identify and correct zero errors before taking measurements.
When taking measurements, it is essential to consider the accuracy and precision of the measuring instrument, as these factors impact the reliability of the data collected. Additionally, environmental conditions, such as temperature and humidity, can affect measurements and should be controlled or noted. Proper technique and consistency in measurement methods are also crucial to ensure valid comparisons and results. Lastly, always account for potential sources of error and uncertainty in the measurement process.
Ensure the measuring instrument is calibrated and in good working condition. Take measurements in a controlled environment to minimize external factors that could affect the accuracy of the measurement. Follow standardized procedures and guidelines to ensure consistency and reliability in the measurements. Take multiple measurements and calculate the average to reduce the risk of errors.
To overcome density experiment, you can try using a more precise measuring instrument for weighing and volume measurements, ensuring all measurements are taken at the same temperature and pressure, and repeating the experiment multiple times to account for any errors or inconsistencies. Additionally, ensuring proper mixing and handling of the materials before taking measurements can help improve accuracy.
Uncertainty in physics measurements can be determined by calculating the range of possible values around the measured quantity, taking into account factors such as instrument precision, human error, and environmental conditions. This is typically done using statistical methods like standard deviation or error propagation.
Taking accurate measurements in a workshop.
An astrolabe is an ancient navigation instrument used to measure the altitude of celestial bodies, typically used for determining latitude and telling time. It consists of a disk with a rotating arm and sights for taking measurements of the stars and planets.