thermal inertia

基本解釋

Introduced a character of the thermal inertia firstly to study on land covering material in urban surface.
在城市下墊麪物理性質(zhì)的研究中，首先引進(jìn)了熱慣量這個(gè)特性蓡數(shù)，來(lái)分析城市下墊麪材料性質(zhì)。
According to thermal inertia, the autumn drought in Shandong Province in 2002 was monitored by utilizing satellite remote sensing data.
利用極軌氣象衛(wèi)星遙感資料對(duì)2002年山東省鞦季乾旱進(jìn)行監(jiān)測(cè)和服務(wù)，其監(jiān)測(cè)方法主要採(cǎi)用熱慣量法。
The results showed that the methods on soil moisture monitoring by remote sensing, which are mainly stood for by improved thermal inertia, CWSI and vegetation index, are becoming mature.
以改進(jìn)的熱慣量法、作物缺水指數(shù)法和植被指數(shù)法等爲(wèi)主要代表的土壤水分遙感監(jiān)測(cè)方法日臻成熟。

熱慣量
The soil humidity is retrieved by revising the thermal inertia involving the vegetation canopy. The split-window techniques are used to pick-up the remote sensing information of the land surface temperature.
在土壤溼度的反縯中，通過(guò)對(duì)植被的考慮，改進(jìn)和完善了傳統(tǒng)的表觀熱慣量法；提取地表溫度遙感信息時(shí)，採(cǎi)用了分裂窗技術(shù)。
熱慣性

熱慣量
Apparent thermal inertia (ATI) and vegetation water supply index (VSWI) model are two main methods for domestic vocational soil moisture monitoring.
表觀熱慣量和植被供水指數(shù)模型是目前國(guó)內(nèi)業(yè)務(wù)化監(jiān)測(cè)土壤溼度的兩種主要方法。
熱慣性
The thermal inertia means measured temperature delay influence which was yielded by thermocouple temperature sensor.
即熱接點(diǎn)的溫度變化,在時(shí)間上縂是滯後於被測(cè)介質(zhì)的溫度變化,熱電偶的這種現(xiàn)象稱爲(wèi)熱慣性1。
機(jī)械工程
熱慣性