新竹縣 Live Rainfall

Latest automatic rainfall station observations in 新竹縣.

Source: Central Weather Administration Open Data Platform

Observed at: 09/18/2026 13:10Processed at: 09/18/2026 13:21

Stations

53

Stations with rain

0

Max 1-hour rainfall

0.0 mm

五峰國小

Max daily rainfall

0.0 mm

五峰國小

Live rainfall highlights

Use the latest one-hour observations to quickly understand rainfall conditions across Taiwan.

No notable rain

No station in 新竹縣 recorded notable rainfall during the latest hour. Check the 3- and 24-hour totals for recent accumulation.

1-hour rain coverage0.0%0 / 53 stations

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Highest rainfall stations

Top 15 stations for the selected rainfall interval.

Stations in 新竹縣

Showing 53 stations

StationLocation1 hour3 hours12 hours24 hours
五峰國小新竹縣五峰鄉0.00.00.00.0
大坪苗圃新竹縣五峰鄉0.00.00.00.0
太閣南新竹縣五峰鄉0.00.00.00.0
太閣南新竹縣五峰鄉0.00.00.00.0
桃改五峰分場新竹縣五峰鄉0.00.00.00.0
樂山林道6k新竹縣五峰鄉0.00.00.00.0
清泉新竹縣五峰鄉0.00.00.00.0
白蘭新竹縣五峰鄉0.00.00.00.0
石鹿新竹縣五峰鄉0.00.00.00.0
花園派出所新竹縣五峰鄉0.00.00.00.0
雪霸新竹縣五峰鄉0.00.00.00.0
外坪五指新竹縣北埔鄉0.00.00.00.0
國一S098K新竹縣寶山鄉0.00.00.00.0
國一S105K新竹縣寶山鄉0.00.00.00.0
寶山新竹縣寶山鄉0.00.00.00.0
寶山農場新竹縣寶山鄉0.00.00.00.0
新城國小新竹縣寶山鄉0.00.00.00.0
尖石國小新竹縣尖石鄉0.00.00.00.0
梅花新竹縣尖石鄉0.00.00.00.0
梅花新竹縣尖石鄉0.00.00.00.0
玉峰新竹縣尖石鄉0.00.00.00.0
田埔分校新竹縣尖石鄉0.00.00.00.0
白石新竹縣尖石鄉0.00.00.00.0
秀巒國小新竹縣尖石鄉0.00.00.00.0
西丘斯山新竹縣尖石鄉0.00.00.00.0
錦屏國小新竹縣尖石鄉0.00.00.00.0
鎮西堡新竹縣尖石鄉0.00.00.00.0
鳥嘴山新竹縣尖石鄉0.00.00.00.0
鳥嘴山新竹縣尖石鄉0.00.00.00.0
峨眉新竹縣峨眉鄉0.00.00.00.0
巨埔新竹縣新埔鎮0.00.00.00.0
打鐵坑新竹縣新埔鎮0.00.00.00.0
新埔新竹縣新埔鎮0.00.00.00.0
新埔(1)新竹縣新埔鎮0.00.00.00.0
桃改新埔分場新竹縣新埔鎮0.00.00.00.0
外湖新竹縣新豐鄉0.00.00.00.0
新豐新竹縣新豐鄉0.00.00.00.0
西濱N060K新竹縣新豐鄉0.00.00.00.0
內灣國小新竹縣橫山鄉0.00.00.00.0
橫山新竹縣橫山鄉0.00.00.00.0
國一N077K新竹縣湖口鄉0.00.00.00.0
國一S082K新竹縣湖口鄉0.00.00.00.0
湖口新竹縣湖口鄉0.00.00.00.0
國一S088K新竹縣竹北市0.00.00.00.0
新竹新竹縣竹北市0.00.00.00.0
竹東新竹縣竹東鎮0.00.00.00.0
飛鳳山新竹縣芎林鄉0.00.00.00.0
國三N077K新竹縣關西鎮0.00.00.00.0
國三N085K新竹縣關西鎮0.00.00.00.0
錦山國小新竹縣關西鎮0.00.00.00.0
關西新竹縣關西鎮0.00.00.00.0
關西(3)新竹縣關西鎮0.00.00.00.0
關西工作站新竹縣關西鎮0.00.00.00.0

Rainfall FAQ and interpretation

Understand rainfall units, regional navigation, and how to use station observations correctly.

FAQ

The primary factor is the "orographic lift effect" combined with windward and leeward slope dynamics.

When humid monsoon air masses (such as the summer southwest monsoon or winter northeast monsoon) encounter mountain ranges in 新竹縣, moisture is forced aloft and condenses into dense precipitation clouds.

Consequently, mountainous catchment areas often experience several times the precipitation recorded along low-lying coastal plains.