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rainy season unified rainy season monitoring system standard empty rainy season rainy season length qx/t series rainy season monitoring standards routine reliability test reliability test organic water chemistry analysis method technology evolution analysis compared gigabit ethernet switches
QX/T 495-2019 in English

QX/T 495-2019 in English

VALID

Monitoring indices of rainy season in China-Rainy season in North China

  • Issued on:2019-09-18
  • Implemented on:2019-12-01
  • File Format:PDF
  • Delivery:Via email within 1~3 business days
Price(USD): $220.00
$214.00
Standard No: QX/T 495-2019
Document status: VALID
Title in English: Monitoring indices of rainy season in China-Rainy season in North China
Title in Chinese: 中国雨季监测指标 华北雨季
Language: English
File Format: Electronic (PDF)
Delivery: Via email within 1~3 business days
Issued on: 2019-09-18
Implemented on: 2019-12-01
Professional Classification: QX-Meteorology
Related Keywords: rainy season
unified rainy season monitoring system
standard empty rainy season
rainy season length
qx/t series rainy season monitoring standards
Related Topics: Chinese standard
China
chinese winter
Zhou Zhonghua
rain
american rainwater
moderate rain
North China
North test detection
Canned Chinese
Chinese measurement
North China Permian
China Test China Test
Tsubaki Zhonghua
China Indicators
Chinese cadmium index
North China Jurassic
Huake Guozhong
China Surveying Network
Hua Guoqiang
South China Beihang Airlines
Total nickel in rainwater
Microplastic monitoring in China
Beikang Testing International
First level national standard monitoring


Introduction

Standard Framework and Technology Evolution

This standard, as a northern regional supplement to the QX/T series rainy season monitoring standards, establishes a unified rainy season monitoring system in North China (Beijing-Tianjin-Hebei, Shanxi, and Inner Mongolia) for the first time. Compared with the traditional empirical judgment method proposed by Zhao Hanguang in 1994, it innovatively introduces a dual-factor judgment model of the position of the subtropical high pressure ridgeline in the northwest Pacific and precipitation.


Analysis of core monitoring indicators

Indicator typeBeijing-Tianjin-Hebei standardShanxi standardInner Mongolia standard
Starting threshold5-day precipitation ≥35mm and single-day ≥10mmSame as Beijing-Tianjin-Hebei5-day precipitation ≥25mm and single-day ≥10mm
Ending threshold5-day precipitation ≤35mm in 10 consecutive daysSame as Beijing-Tianjin-Hebei5-day precipitation ≤25mm in 10 consecutive days
Station ratio thresholdStart 70%/End 60%Start 60%/End 60%Start 50%/End 50%

Intensity classification system

Precipitation level (Formula Z=(P-P₀)/S)

Typical case: In 2016, the Z value of the rainy season in North China reached 2.1, which was a significantly higher level (Ip=5), and the actual precipitation was 120% higher than the climate average

Comprehensive intensity index (Formula M)

Includes three dimensions: relative value of rainy season length (L/L₀), daily precipitation intensity ratio, and precipitation ratio. The critical value 1.25 is the boundary between strong and weak


Mechanism for handling special situations

  • Delayed rainy season: When the starting day is later than August 10, the first precipitation day exceeding the climate mean is taken
  • Empty rainy season: In 2014, a standard empty rainy season (annual precipitation <100mm) occurred in the monitoring area of Inner Mongolia

Implementation recommendations

  1. Data quality control: It is recommended to combine automatic weather stations with manual observation data
  2. Climate benchmark update: According to WMO regulations, the 1981-2010 benchmark value is updated every 10 years
  3. Regional application: The monitoring area of Inner Mongolia needs to pay special attention to grassland ecological impact assessment

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