Aktualna faza Księżyca na dziś i tę noc to Ubywający sierp. Księżyc jest teraz oświetlony w 13.8 % i jest ubywający. Marzec 4, 2027Dziś Księżyc ma 26.0 dni.
Przybliżona odległość Ziemi od Księżyca wynosi 404,343, a do następnej fazy pozostało 3.9 dni – (Nów).
Odwiedź także Marzec 2027 Kalendarz faz Księżyca, aby zobaczyć wszystkie dzienne fazy Księżyca w tym miesiącu.
Faza Księżyca: Ubywający sierp
Poprzednia faza: Ostatnia kwadra ()
Odległość Księżyca: 404,343 km
Oświetlenie: 13.8 %
Wiek Księżyca: 26.0 dni
Następna faza: Nów ()
Rozmiar kątowy Księżyca: 0.49
Odległość Słońca: 148,326,974 km
Znak zodiaku Księżyca: Wodnik
2027-02-06 – 2027-03-08
| Faza Księżyca | DATA I GODZINA |
DATA I GODZINA (UTC) |
|---|---|---|
| Nów | ||
| Pierwsza kwadra | ||
| Pełnia | ||
| Ostatnia kwadra | ||
| Nów |
To pierwsza i niewidoczna faza Księżyca – oświetlona strona Księżyca zwrócona jest ku Słońcu, a nocna ku Ziemi. Nów jest bezpośrednio widoczny tylko podczas zaćmienia Słońca.
Pierwsza kwadra
Tydzień po nowiu następuje pierwsza kwadra, gdy Księżyc przebył ćwierć swojej orbity. Nazywana jest też półksiężycem. Księżyc w pierwszej kwadrze wschodzi około południa i zachodzi około północy.
Pełnia
Przy 100 % oświetlenia dzienna strona Księżyca jest zwrócona wprost ku nocnej stronie Ziemi i Księżyc jest w pełni. Pełnia wschodzi o zachodzie Słońca i zachodzi o wschodzie, a przy horyzoncie wydaje się większa.
Ostatnia kwadra
Księżyc wchodzi w ostatnią (trzecią) kwadrę swojej orbity w wieku prawie 23 dni. Oświetlona wydaje się tylko połowa. Tę fazę widać późną nocą i wczesnym rankiem (około 6).
The Moon crust is made of composed primarily of oxygen (O), silicon (Si), magnesium (Mg), iron (Fe), calcium (Ca), and aluminum (Al), but important minor and trace elements such as titanium (Ti), uranium (U), thorium (Th), potassium (K), and hydrogen (H) are present as well. Below the crust is the mantle coming, with a thickness of roughly 1350 km is far more extensive than the crust, which has an average thickness of about 50 km. The mantle is made of olivine, orthopyroxene and clino pyroxene. Finally, at the center is the Moon’s dense, metallic core. The core is largely composed of iron (Fe) and some nickel (Ni). The inner core is a solid mass of about 480 km in diameter. Surrounding the solid inner core is a fluid outer core, that brings the total diameter of the core to about 660 km.
Więcej Fakty o KsiężycuThis is an optical illusion. The Moon looks large shortly after it rises when it's still touching the horizon. This is not the same as a Supermoon.
Więcej Fakty o KsiężycuHere are the top 5 things that make the Moon so unique.
1. The Moon is Earth's only permanent natural satellite.
2. Moon dust smells like gunpowder.
3. The Moon keeps the same face pointing toward the Earth.
4. The Moon has no – or just a really thin – atmosphere so there is no weather.
5. The Moon is visible in daylight nearly every day.
A supermoon occurs when the Moon's orbit is closest (perigee) to Earth at the same time the Moon is full. At such a time, the Moon can look larger and brighter than it normally does - especially when it is seen rising above the horizon. However, it's important to note that the actual difference in size and brightness between a supermoon and an average full moon is not typically dramatic, and may not be noticeable to the naked eye without a direct comparison.
Więcej Fakty o KsiężycuNo, the moon has no water and has only a very thin and tenuous atmosphere (called an exosphere) so it cannot trap heat or insulate the surface. So, for example, there is no wind to create weather system. The Moon does, in fact, affect the Earth's climate and weather patterns in several subtle ways.
Więcej Fakty o KsiężycuAn analysis of moon's mineral composition suggests that the moon is around 4.425 billion years old.
Więcej Fazy KsiężycaThe Moon crust is made of composed primarily of oxygen (O), silicon (Si), magnesium (Mg), iron (Fe), calcium (Ca), and aluminum (Al), but important minor and trace elements such as titanium (Ti), uranium (U), thorium (Th), potassium (K), and hydrogen (H) are present as well. Below the crust is the mantle coming, with a thickness of roughly 1350 km is far more extensive than the crust, which has an average thickness of about 50 km. The mantle is made of olivine, orthopyroxene and clino pyroxene. Finally, at the center is the Moon’s dense, metallic core. The core is largely composed of iron (Fe) and some nickel (Ni). The inner core is a solid mass of about 480 km in diameter. Surrounding the solid inner core is a fluid outer core, that brings the total diameter of the core to about 660 km.
Więcej Fazy KsiężycaNo, it doesn’t generate its own light. “Moonlight” is really sunlight that has reflected off of the Moon’s surface. In the same way that the Sun illuminates Earth, the Moon reflects the Sun's light, making it appear bright in our sky.
Więcej Fazy KsiężycaA "micromoon" is a term used in popular astronomy to describe a full moon or a new moon that occurs when the moon is at or near its apogee, which is the furthest point from Earth in its elliptical orbit. This is the opposite of a "supermoon," which occurs when a full moon or new moon is at or near its perigee, which is the closest point to Earth in its orbit."
Więcej Fazy KsiężycaNo, the moon has no water and has only a very thin and tenuous atmosphere (called an exosphere) so it cannot trap heat or insulate the surface. So, for example, there is no wind to create weather system. The Moon does, in fact, affect the Earth's climate and weather patterns in several subtle ways.
Więcej Fazy KsiężycaAn orange moon means the shorter wavelengths of light are being filtered away. This could be due to the low position on the horizon causing the light to go through more atmosphere, smoke in the air, or pollution.
Więcej CiekawostkiThis is an optical illusion. The Moon looks large shortly after it rises when it's still touching the horizon. This is not the same as a Supermoon.
Więcej CiekawostkiThe Moon makes Earth a more livable planet by moderating our home planet's wobble on its axis, leading to a relatively stable climate.
Więcej CiekawostkiThe Moon crust is made of composed primarily of oxygen (O), silicon (Si), magnesium (Mg), iron (Fe), calcium (Ca), and aluminum (Al), but important minor and trace elements such as titanium (Ti), uranium (U), thorium (Th), potassium (K), and hydrogen (H) are present as well. Below the crust is the mantle coming, with a thickness of roughly 1350 km is far more extensive than the crust, which has an average thickness of about 50 km. The mantle is made of olivine, orthopyroxene and clino pyroxene. Finally, at the center is the Moon’s dense, metallic core. The core is largely composed of iron (Fe) and some nickel (Ni). The inner core is a solid mass of about 480 km in diameter. Surrounding the solid inner core is a fluid outer core, that brings the total diameter of the core to about 660 km.
Więcej CiekawostkiThe Moon is the fifth largest satellite in the Solar System and the biggest in comparison to its host planet, with a diameter about one-quarter that of Earth. The exact diameter is 2159.14 miles (3 474.8 km ).
Więcej Ciekawostki
MoonPhaseToday.org pozwala sprawdzić fazę Księżyca na dziś i tę noc, a także na dowolny dzień, miesiąc i rok. Obliczenia fazy Księżyca opierają się na Twojej strefie czasowej, ale pokazujemy też dokładne godziny w formacie UTC. Mamy nadzieję, że nasze narzędzie okaże się przydatne i wygodne w sprawdzaniu faz Księżyca.
MoonPhaseToday.org