Pomelo is very large citrus fruit of botanical name Citrus maxima. It is very sweet taste after ripening . Have you ever tried a honey pomelo ? This large citrus fruit can be found in the produce section from late fall to early spring. Here's more about this tasty unique citrus fruit.The fruit is used in many festive celebrations throughout Southeast Asia. After a Captain Shaddock of an East India Company ship introduced it to Barbados, the fruit was called "shaddock" in English. The fruit is also known as jabong in Hawaii and jambola in varieties of English spoken in South Asia. The etymology of the word "pomelo" is uncertain. It may be an alteration of "pompelmoes", in Tamil pomelo are called pampa limasu, which means "big citrus". The name was adopted by the Portuguese as pomposos limoes and then by the Dutch as pompelmoes. Typically, the fruit is pale green to yellow when ripe, with sweet white ( or, more rarely , pink or red) fle...
Spring is heading this year with beautiful flowers. Spring, also known as springtime is one of the four temperate seasons, following winter and preceding summer. There are various technical definitions of spring, but local usage of the term varies according to local climate, cultures and customs. When it is spring in the Northern Hemisphere, it is autumn in the Southern Hemisphere and vice versa. At the spring (or vernal) equinox, days and nights are approximately twelve hours long, with day length increasing and night length decreasing as the season progresses. Spring and springtime refer to the season, and also to ideas of rebirth, rejuvenation, renewal, resurrection and regrowth. Subtropical and tropical areas have climates better described in terms of other seasons, e.g. dry or wet, monsoonal or cyclonic. Cultures may have local names for seasons which have little equvalence to the terms originating in Europe.
Weather forecast
Meteorologists typically define four seasons in several climatic zones: spring, summer, autumn (fall) and winter. These are delimited by their average temperature values on a monthly basis, with each season lasting for three months. The three wettest months are by definition summer, the three coldest months are winter and the intervals between are spring and autumn. Spring, when defined in this manner, can begin on different dates in different regions.
Thus, in the US and UK, the spring months are March, April and May, while in New Zealand and Australia, spring traditionally starts from September 1 and ends on November 30. it happens.
Swedish meteorologists have defined the beginning of spring as the first occasion on which the average daytime temperature exceeds zero degrees Celsius for seven consecutive days, thus the date varies with latitude and altitude.
In some cultures in the Northern Hemisphere (eg Germany), the celestial Vériel equinox (the difference between 19 and 21 March) is taken to mark the first day of spring, and the summer solstice (about 21 June) as the first day. Is taken in heat. In Persian culture the first day of spring is the first day of the first month (called Farwardine) that begins on 20 or 21 March. In other traditions, the equinox is taken as mid-spring.
In the traditional Chinese calendar, the "spring" season (consists) consists of days between Lichun (February 3–5), taking Chinaphen (March 20–20) as its midpoint, then Lixia (5–7) May) ends. Similarly, according to Celtic tradition, which is based entirely on the strength of daylight and afternoon sun, spring begins in early February (near Imbolak or Candlemas) and continues until early May (Belton) is.
Ecological calculation
The beginning of spring is not always determined by fixed calendar dates. The phenological or ecological definition of spring is related to biological indicators, such as the blooming of a range of plant species, animal movements, and the characteristic odor of soil that has reached the temperature of micro-flora to thrive. These indicators vary with the onset of spring, according to the local climate and the specific season of a particular year. Some ecologists divide the year into six seasons. In addition to spring, the ecological reckoning identifies predetermined (early or pre-spring) seasons as distinct from those between the hibernal (winter) and vernal (spring) seasons. This is a time when only the hardest flowers like crocus bloom, sometimes while there is still some snow on the ground.
During the early spring, the Earth's axis is increasing its inclination relative to the Sun, and the length of daylight increases rapidly for the relevant hemisphere. The hemisphere begins to heat up considerably, causing the growth of the new plant "towards spring", which gives the weather its name.
Any ice begins to melt, swollen streams with runoff and any frost become less severe. In climates that have no snow, and rare frost, wind and ground temperatures rise rapidly.
Many flowering plants bloom at this time of year, in a long succession, sometimes beginning when snow is still on the ground and continuing into early summer. In generally snow-free areas, the "spring" may begin as February (Northern Hemisphere) or August (Southern Hemisphere), heralded by the blooming of deciduous magnolia, cherries and quince. Many temperate regions have a dry spring, and a wet autumn (autumn), which is more consistent with warmth, along with the need for water to bring flowers in this season. Subarctic areas may not experience "spring" until May.
While spring is the result of heat caused by the changing orientation of the Earth's axis relative to the Sun, weather in many parts of the world is affected by other, less predictable events. Rainfall in spring (or any season) follows trends related to more long cycles - such as solar cycles - or events created by ocean currents and ocean temperatures - for example, the El Niño effect and the Southern Oscillation Index.
The unstable spring weather may occur more frequently when warmer air begins to invade from lower latitudes, while colder air is still thrusting from polo fields. Flooding is also most common in and near mountainous areas during this time of the year, as rainfall is less due to snowfall. In North America, the Tornado Alley is the most active at this time of year, especially since the Rocky Mountains prevent rising hot and cold air masses from spreading eastward, and instead force them into direct conflict. In addition to tornadoes, supercell thunderstorms can also produce dangerously large hail and very strong winds, for which a strong thunderstorm or storm warning is usually issued. Even more than in winter, jet streams play an important role in the unstable and severe northern hemisphere seasons in spring.
In recent decades, season creep has been observed, meaning that many phenological signs of spring are occurring in many areas around the first two per decade. [Citation needed]
Spring in the Southern Hemisphere differs from the Northern Hemisphere in several important ways for several reasons, including:
There is no land bridge between the Southern Hemisphere countries and the Antarctic region capable of bringing cold air without the temperature-quenching effect of a wide tract of water;
Vast amounts of ocean in the southern hemisphere at most latitudes;
At this time in Earth's geological history there is an orbit of the Earth that brings it closer to the Southern Hemisphere for its warmer weather;
The uninterrupted air flow from a large land mass is the flow (roaring 40s and 50s);
No equivalent jet currents; And
Feature of reversed ocean currents in the Pacific.
Weather forecast
Meteorologists typically define four seasons in several climatic zones: spring, summer, autumn (fall) and winter. These are delimited by their average temperature values on a monthly basis, with each season lasting for three months. The three wettest months are by definition summer, the three coldest months are winter and the intervals between are spring and autumn. Spring, when defined in this manner, can begin on different dates in different regions.
Thus, in the US and UK, the spring months are March, April and May, while in New Zealand and Australia, spring traditionally starts from September 1 and ends on November 30. it happens.
Swedish meteorologists have defined the beginning of spring as the first occasion on which the average daytime temperature exceeds zero degrees Celsius for seven consecutive days, thus the date varies with latitude and altitude.
In some cultures in the Northern Hemisphere (eg Germany), the celestial Vériel equinox (the difference between 19 and 21 March) is taken to mark the first day of spring, and the summer solstice (about 21 June) as the first day. Is taken in heat. In Persian culture the first day of spring is the first day of the first month (called Farwardine) that begins on 20 or 21 March. In other traditions, the equinox is taken as mid-spring.
In the traditional Chinese calendar, the "spring" season (consists) consists of days between Lichun (February 3–5), taking Chinaphen (March 20–20) as its midpoint, then Lixia (5–7) May) ends. Similarly, according to Celtic tradition, which is based entirely on the strength of daylight and afternoon sun, spring begins in early February (near Imbolak or Candlemas) and continues until early May (Belton) is.
Ecological calculation
The beginning of spring is not always determined by fixed calendar dates. The phenological or ecological definition of spring is related to biological indicators, such as the blooming of a range of plant species, animal movements, and the characteristic odor of soil that has reached the temperature of micro-flora to thrive. These indicators vary with the onset of spring, according to the local climate and the specific season of a particular year. Some ecologists divide the year into six seasons. In addition to spring, the ecological reckoning identifies predetermined (early or pre-spring) seasons as distinct from those between the hibernal (winter) and vernal (spring) seasons. This is a time when only the hardest flowers like crocus bloom, sometimes while there is still some snow on the ground.
During the early spring, the Earth's axis is increasing its inclination relative to the Sun, and the length of daylight increases rapidly for the relevant hemisphere. The hemisphere begins to heat up considerably, causing the growth of the new plant "towards spring", which gives the weather its name.
Any ice begins to melt, swollen streams with runoff and any frost become less severe. In climates that have no snow, and rare frost, wind and ground temperatures rise rapidly.
Many flowering plants bloom at this time of year, in a long succession, sometimes beginning when snow is still on the ground and continuing into early summer. In generally snow-free areas, the "spring" may begin as February (Northern Hemisphere) or August (Southern Hemisphere), heralded by the blooming of deciduous magnolia, cherries and quince. Many temperate regions have a dry spring, and a wet autumn (autumn), which is more consistent with warmth, along with the need for water to bring flowers in this season. Subarctic areas may not experience "spring" until May.
While spring is the result of heat caused by the changing orientation of the Earth's axis relative to the Sun, weather in many parts of the world is affected by other, less predictable events. Rainfall in spring (or any season) follows trends related to more long cycles - such as solar cycles - or events created by ocean currents and ocean temperatures - for example, the El Niño effect and the Southern Oscillation Index.
The unstable spring weather may occur more frequently when warmer air begins to invade from lower latitudes, while colder air is still thrusting from polo fields. Flooding is also most common in and near mountainous areas during this time of the year, as rainfall is less due to snowfall. In North America, the Tornado Alley is the most active at this time of year, especially since the Rocky Mountains prevent rising hot and cold air masses from spreading eastward, and instead force them into direct conflict. In addition to tornadoes, supercell thunderstorms can also produce dangerously large hail and very strong winds, for which a strong thunderstorm or storm warning is usually issued. Even more than in winter, jet streams play an important role in the unstable and severe northern hemisphere seasons in spring.
In recent decades, season creep has been observed, meaning that many phenological signs of spring are occurring in many areas around the first two per decade. [Citation needed]
Spring in the Southern Hemisphere differs from the Northern Hemisphere in several important ways for several reasons, including:
There is no land bridge between the Southern Hemisphere countries and the Antarctic region capable of bringing cold air without the temperature-quenching effect of a wide tract of water;
Vast amounts of ocean in the southern hemisphere at most latitudes;
At this time in Earth's geological history there is an orbit of the Earth that brings it closer to the Southern Hemisphere for its warmer weather;
The uninterrupted air flow from a large land mass is the flow (roaring 40s and 50s);
No equivalent jet currents; And
Feature of reversed ocean currents in the Pacific.
Comments
Post a Comment