on May 27, 2024
Evaluating the Accuracy of T-phigram Satellite-Derived Soundings Compared to Model Output
RadiosoundingIntroduction to T-phigram Satellite Derived Soundings In the field of atmospheric science, the analysis and interpretation of vertical atmospheric profiles is critical to understanding weather patterns, climate change, and a wide range of environmental processes. One of the key tools in this endeavor is the use of satellite-derived soundings, which provide valuable insights into the
on December 17, 2023
Unveiling Atmospheric Stability: Exploring CAPE Calculation for Accurate Radiosounding Analysis
RadiosoundingUnderstanding CAPE Calculation in Radiosounding and Earth Science Introduction to CAPE In the field of meteorology and atmospheric science, Convective Available Potential Energy (CAPE) is a critical parameter used to assess the potential for atmospheric instability and the likelihood of thunderstorm development. CAPE plays an important role in weather forecasting, helping meteorologists predict severe weather
on September 19, 2023
Unlocking the Secrets of Earth’s Atmosphere: Advancements in High Vertical Resolution Radiosounding Data
RadiosoundingGetting Started Atmospheric sounding, also known as radiosounding, is a fundamental technique used in Earth science to study the vertical profile of the atmosphere. It involves the measurement of various atmospheric parameters such as temperature, humidity, pressure and wind speed at different altitudes. These measurements provide valuable insights into the structure and dynamics of the
on June 1, 2023
Extreme temperatures at the stratopause: record-breaking highs and lows revealed through radiosounding
RadiosoundingThe stratopause is a layer of the Earth’s atmosphere that separates the stratosphere from the mesosphere. It is located at an altitude of about 50-55 km (31-34 miles) above the Earth’s surface. The temperature at the stratopause is of great interest to scientists because it plays an important role in the dynamics of the upper