The lowest atmospheric pressure ever recorded on Earth occurred during Typhoon Tip in the western Pacific Ocean in 1979, where the central pressure dropped to approximately 870 millibars (mb) or 25.69 inches of mercury (inHg). This extreme low-pressure system was associated with a very powerful tropical cyclone (typhoon) and is considered the lowest reliably measured sea-level pressure in recorded history.
Regarding the uneven heating of land and water in winter and its impact on rainfall, it's important to understand how seasonal temperature differences affect weather patterns:
Uneven Heating of Land and Water in Winter: During winter, land and water surfaces experience differential heating due to their varying heat capacities and thermal properties:Land Surface: Land cools down more quickly than water during winter nights and retains less heat during the day. Water Surface: Bodies of water, such as oceans and large lakes, have higher heat capacities and retain more warmth compared to land.
Impact on Rainfall: The differential heating between land and water in winter can lead to specific weather patterns that are characterized by relatively less rainfall over land areas:High-Pressure Systems: As land surfaces cool down faster than water, particularly during clear winter nights, areas of high pressure can develop over land. High-pressure systems are generally associated with stable atmospheric conditions and clear skies, inhibiting the development of significant rainfall. Dry Air Masses: Cold air masses originating from land surfaces tend to be drier and have lower moisture content compared to air masses originating from warmer water surfaces. This dry air can further reduce the likelihood of precipitation over land areas in winter. Limited Moisture Source: During winter, the availability of moisture for precipitation is generally lower due to reduced evaporation rates from cooler water surfaces and less convective activity compared to warmer seasons.
Snowfall vs. Rainfall: In regions where temperatures are sufficiently cold, the limited moisture content and stable atmospheric conditions in winter can result in precipitation falling primarily as snow rather than rain. This is especially true in continental climates where cold air masses interact with moisture from nearby bodies of water, leading to the accumulation of snowfall.
In summary, the uneven heating of land and water surfaces in winter contributes to specific weather patterns characterized by lower rainfall over land areas due to the development of high-pressure systems, limited moisture availability, and the prevalence of cold, dry air masses. These factors collectively influence the type and amount of precipitation observed during the winter season.
The lowest atmospheric pressure, barometric pressure, ever recorded was in 1979 within a typhoon in the Pacific Ocean. The air pressure therein measured at 870 millibars or 25.9 in-Hg (inches of mercury). Average air pressure measures about 29.9 inches or around 1013.25 millibars of pressure. The lowest pressures currently achievable in laboratory are about 1×10−13 torrs (13 pPa). However, pressures as low as 5×10−17 torrs (6.7 fPa) have been indirectly measured in a 4 K (−269.15 °C; −452.47 °F) cryogenic vacuum system. Uneven heating of the land during winter generates winds from colder north western areas. These bring rainfall to Tamil Nadu, parts of Andhra, etc. The uneven heating of land and sea water causes monsoon winds. In summer, land becomes warmer than the sea. This causes winds to flow from sea to land and brings moisture with them. During the day, air above land heats up faster than air above water. The uneven heating of land and sea water causes monsoon winds. In summer, land becomes warmer than the sea. This causes winds to flow from sea to land and brings moisture with them. In winter, the direction of the wind gets reversed and there is hardly any moisture in it.
The lowest recorded air pressure on Earth that we can be sure of was measured at sea level and not inside a tornado. This measurement was incredibly low, at only 870 millibars (mb), which is 25.69 inches of mercury. This record was set on October 12, 1979, during Typhoon Tip in the western Pacific Ocean.
There is some debate about an even lower pressure being measured in a different typhoon, but that value hasn't been officially verified.
As for uneven heating of land and water in winter, that's a big contributor to lower winter precipitation in many places. Here's why:
Land cools off much faster than water in the fall and winter.
Colder air holds less moisture, so as the land cools, the air above it dries out.
This dry air masses then move over the bodies of water, which are still relatively warm.
The warm water can't transfer much moisture to the dry air, so there's less rain or snow.