Free / commercial imagery

基础设施热惯量

由昼夜影像对得到的表观热惯量:致密材料对疏松填土。

昼夜热差分,按反照率归一化。致密材料散热比疏松填土慢。

基础设施热惯量
In view

Apparent thermal inertia from a day and night pair: dense material cools slowly, loose fill cools fast.

它能发现什么

它检测什么。

材料典型产出环境可能的混淆因素
Apparent Thermal Inertia (ATI) AnomaliesCivil infrastructure corridors, foundation pads, runway subgrades, and shallow buried utilitiesSurface wind gusts altering convective heat transfer

方法

工作原理。

输入校准反射率,每个像元都对照公开参考库进行拟合。

01Step 1

Pairing a day and a night pass

The midday and pre-dawn acquisitions are placed on a common grid. Both must cover the same ground inside one diurnal cycle, which is the constraint that makes this hard to procure rather than hard to compute.

02Step 2

Broadband albedo

Optical bands are integrated into a broadband albedo, which sets how much solar energy the surface took in during the day.

03Step 3

Apparent thermal inertia

ATI = (1 - α) / (T_day - T_night). The word apparent is load-bearing: this is a proxy for heat capacity and conductivity, not a measurement of either.

04Step 4

Segmentation into high and low inertia

Dense material separates from loose fill. What causes the contrast is an interpretation the map cannot make for you.

技术规格

您得到什么,它在什么数据上运行。

交付数值Apparent thermal inertia, floating point, unitless
输出Apparent thermal inertia surface
交付周期Set by the day and night acquisition window, not by processing
格式
Cloud-Optimized GeoTIFF (COG)Vector Thermal Contours (GeoJSON)Provenance record (both acquisition times in UTC, method version)

所需环境条件

Sun angle limit:50°
Cloud cover limit:0%
Vegetation cover limit:20%

Method and checks are documented in Axine Applied Spectroscopy Technical Whitepaper · Series 5.

阅读论文

适用边界

Both passes have to be cloud-free and calm. Wind at night masks the signal this depends on.

在您的土地上运行

在您自己的区域运行这个图层。

为您的感兴趣区(AOI)订购处理,或在影像库无可用数据时订购定制拍摄。影像访问永不收费:方案购买的是模型。

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