Skip to main content

low pass filter in remote sensing

A low pass filter is a type of filter that allows low frequency signals to pass through, while blocking or attenuating high frequency signals.

In remote sensing, low pass filters are often used to remove noise or other high frequency interference from the acquired data.

Low pass filters are commonly used in multispectral and hyperspectral imaging sensors to eliminate noise and improve signal to noise ratio.

Low pass filters can be implemented in both hardware and software. Hardware filters are typically installed in the sensor itself, while software filters can be applied to the acquired data during post-processing.

Low pass filters can be designed with different cut-off frequencies, which determines the range of frequencies that are allowed to pass through the filter.

The use of low pass filters can reduce the spatial resolution of the acquired data, as high frequency signals that contribute to fine details in the image are removed.

Low pass filters can also reduce the contrast of an image by reducing the difference in intensity between adjacent pixels.

There are several different types of low pass filters, including moving average filters, median filters, and Gaussian filters.

Moving average filters work by calculating the average value of a set of adjacent pixels and replacing the original pixel value with the average.

Median filters work by selecting the median value of a set of adjacent pixels and replacing the original pixel value with the median.

Gaussian filters use a Gaussian function to weight the contribution of each pixel to the filtered value, with pixels closer to the center of the kernel contributing more than those further away.

The choice of low pass filter type and cut-off frequency depends on the characteristics of the acquired data and the desired level of noise reduction and spatial resolution.

Low pass filters can be used in combination with other image processing techniques, such as edge detection, to improve the quality and interpretation of remote sensing data.

Low pass filters are commonly used in remote sensing applications such as vegetation mapping, land cover classification, and surface texture analysis.

The use of low pass filters in remote sensing can be limited by the trade-off between noise reduction and spatial resolution, as well as the potential for loss of important high frequency information.





Comments

Popular posts from this blog

geostationary and sun-synchronous

Orbital characteristics of Remote sensing satellite geostationary and sun-synchronous  Orbits in Remote Sensing Orbit = the path a satellite follows around the Earth. The orbit determines what part of Earth the satellite can see , how often it revisits , and what applications it is good for . Remote sensing satellites mainly use two standard orbits : Geostationary Orbit (GEO) Sun-Synchronous Orbit (SSO)  Geostationary Satellites (GEO) Characteristics Altitude : ~35,786 km above the equator. Period : 24 hours → same as Earth's rotation. Orbit type : Circular, directly above the equator . Appears "stationary" over one fixed point on Earth. Concepts & Terminologies Geosynchronous = orbit period matches Earth's rotation (24h). Geostationary = special type of geosynchronous orbit directly above equator → looks fixed. Continuous coverage : Can monitor the same area all the time. Applications Weather...

Disaster Management

1. Disaster Risk Analysis → Disaster Risk Reduction → Disaster Management Cycle Disaster Risk Analysis is the first step in managing disasters. It involves assessing potential hazards, identifying vulnerable populations, and estimating possible impacts. Once risks are identified, Disaster Risk Reduction (DRR) strategies come into play. DRR aims to reduce risk and enhance resilience through planning, infrastructure development, and policy enforcement. The Disaster Management Cycle then ensures a structured approach by dividing actions into pre-disaster, during-disaster, and post-disaster phases . Example Connection: Imagine a coastal city prone to cyclones: Risk Analysis identifies low-lying areas and weak infrastructure. Risk Reduction includes building seawalls, enforcing strict building codes, and training residents for emergency situations. The Disaster Management Cycle ensures ongoing preparedness, immediate response during a cyclone, and long-term recovery afterw...

Disaster Risk

Disaster Risk 

Evaluation and Characteristics of Himalayas

Time Period Event / Process Geological Evidence Key Terms & Concepts Late Precambrian – Palaeozoic (>541 Ma – ~250 Ma) India part of Gondwana , north bordered by Cimmerian Superterranes, separated from Eurasia by Paleo-Tethys Ocean . Pan-African granitic intrusions (~500 Ma), unconformity between Ordovician conglomerates & Cambrian sediments. Gondwana, Paleo-Tethys Ocean, Pan-African orogeny, unconformity, granitic intrusions, Cimmerian Superterranes. Early Carboniferous – Early Permian (~359 – 272 Ma) Rifting between India & Cimmerian Superterranes → Neotethys Ocean formation. Rift-related sediments, passive margin sequences. Rifting, Neotethys Ocean, passive continental margin. Norian (210 Ma) – Callovian (160–155 Ma) Gondwana split into East & West; India part of East Gondwana with Australia & Antarctica. Rift basins, oceanic crust formation. Continental breakup, East Gondwana, West Gondwana, oceanic crust. Early Cretaceous (130–125 Ma) India broke fr...

Discrete Detectors and Scanning mirrors Across the track scanner Whisk broom scanner.

Multispectral Imaging Using Discrete Detectors and Scanning Mirrors (Across-Track Scanner or Whisk Broom Scanner) Multispectral Imaging:  This technique involves capturing images of the Earth's surface using multiple sensors that are sensitive to different wavelengths of electromagnetic radiation.  This allows for the identification of various features and materials based on their spectral signatures. Discrete Detectors:  These are individual sensors that are arranged in a linear or array configuration.  Each detector is responsible for measuring the radiation within a specific wavelength band. Scanning Mirrors:  These are optical components that are used to deflect the incoming radiation onto the discrete detectors.  By moving the mirrors,  the sensor can scan across the scene,  capturing data from different points. Across-Track Scanner or Whisk Broom Scanner:  This refers to the scanning mechanism where the mirror moves perpendicular to the direction of flight.  This allows for t...