
英:/'hɪp'sɒmɪtrɪ/ 美:/'hɪpˈsɑːmətri/
n. [測] 測高法
n.|altimetry;[測]測高法
Hypsometry(測高法)是測量陸地或地形海拔高度的科學方法,主要用于地理學、地質學等領域。以下是詳細解釋:
基本定義
Hypsometry源自希臘語“hypsos”(高度)和“metron”(測量),指通過技術手段确定地表某點相對于海平面的垂直高度。例如,繪制山脈高程或分析盆地地形時常用此方法。
發音與拼寫
音标為英式[hɪp'sɒmɪtrɪ]、美式[hɪp'sɑːmətriː],名詞形式為“hypsometer”(測高儀)。
應用與分類
相關術語
同義詞為“hypsography”(高程測量學),但後者更側重地形高程的圖示表達。
若需了解具體測量工具或不同技術的原理,可進一步查閱地理測量專業文獻。
詞性: 名詞
發音: /haɪpsɑːmətri/
定義: Hypsometry refers to the measurement and mapping of the elevations of land surfaces relative to sea level.
用法: Hypsometry is an important tool for geographers and geologists to study the topography and relief of an area.
解釋: Hypsometry is derived from the Greek word "hypsos" meaning height or altitude, and "metron" meaning measurement. Hypsometry is used to create maps that show the distribution of elevations in a given area. These maps can help scientists understand the topography and relief of an area, as well as its geological history.
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