The Current Local Date and Time in Rain, Germany (DE)
Time Zone Europe/Berlin
08:59:21
Local Time Date and Timezone
Where is Rain? (Germany, DE)
Rain is a city located in Germany (DE).
Latitude 48.69029 Longitude 10.91611
Rain location on the Germany (DE) map
Information about Rain
- City: Rain
- Country: Germany (DE)
- Latitude: 48.69029
- Longitude: 10.91611
- Time Zone: Europe/Berlin
Time zone and UTC offset ofRain
Rain, Germany is in the Europe/Berlin time zone, which is currently UTC+2. This time zone observes daylight saving time (currently in effect). The next clock change is on October 25, 2026.
Current time difference with other cities
- Rain is 1 hour ahead of London
- Rain is 6 hours ahead of New York
- Rain is 9 hours ahead of Los Angeles
- Rain is 2 hours behind Dubai
- Rain is 7 hours behind Tokyo
- Rain is 9 hours behind Sydney
Frequently asked questions about time inRain
What time zone is Rain in?
Rain, Germany is in the Europe/Berlin time zone (currently UTC+2).
Does Rain observe daylight saving time?
Yes, the clocks change during the year in this time zone.
What is the time difference between Rain and New York?
Rain is 6 hours ahead of New York (the difference can change when either place switches to or from daylight saving time).
What are the coordinates of Rain?
Rain is located at latitude 48.69029 and longitude 10.91611.
Sunrise, sunset and moon phase inRain today
Astronomical data for October 16, 2026 in Rain, calculated for the Europe/Berlin time zone. All times are local.
Sun
- Sunrise: 07:38
- Solar noon: 13:02
- Sunset: 18:25
- Length of day: 10 h 47 min
Moon
- Moon phase: Waxing Crescent
- Illumination: 28%
- Moon age: about 5.3 days
- Moonrise: 14:02
- Moonset: 21:23
Other cities inGermany
- Current local time in Berlin
- Current local time in Hamburg
- Current local time in Munich
- Current local time in Koeln
- Current local time in Frankfurt am Main
- Current local time in Stuttgart
- Current local time in Duesseldorf
- Current local time in Essen
- Current local time in Dortmund
- Current local time in Dresden
All cities and towns in Germany
City of Rain
Rain or rainfall is a form of atmospheric precipitation composed of droplets of water aerosols that have condensed from atmospheric water vapor and fall by gravity. Depending on the intensity, rain can be described as a drizzle (very light, sporadic rainfall), a shower (brief, moderate rainfall), a cloudburst (brief heavy rainfall) or a downpour (prolonged heavy or "torrential" rainfall). It is also often accompanied by other weather phenomena such as strong wind (rainstorm) and lightning (thunderstorm), and may be mixed with hail/ice pellet, snow (sleet) and sandstorm (dust rain). Rain is a major component of the water cycle and is responsible for depositing most of the fresh water on Earth. It provides water for hydroelectric power plants, crop irrigation, and suitable conditions for many types of ecosystems.
The major cause of rain production is moisture moving along three-dimensional zones of temperature and moisture contrasts known as weather fronts. If enough moisture and upward motion is present, precipitation falls from convective clouds (those with strong upward vertical motion) such as cumulonimbus (thunder clouds) which can organize into narrow rainbands. In mountainous areas, heavy precipitation is possible where upslope flow is maximized within windward sides of the terrain at elevation which forces moist air to condense and fall out as rainfall along the sides of mountains. On the leeward side of mountains, desert climates can exist due to the dry air caused by downslope flow which causes heating and drying of the air mass. The movement of the monsoon trough, or Intertropical Convergence Zone, brings rainy seasons to savannah climes.
The urban heat island effect leads to increased rainfall, both in amounts and intensity, downwind of cities. Global warming is also causing changes in the precipitation pattern, including wetter conditions across eastern North America and drier conditions in the tropics. The globally averaged annual precipitation over land is 715 mm (28.1 in), but over the whole Earth, it is much higher at 990 mm (39 in). Climate classification systems such as the KΓΆppen classification system use average annual rainfall to help differentiate between differing climate regimes. Rainfall is measured using rain gauges. Rainfall amounts can be estimated by weather radar.
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