The Inter-Tropical Convergence Zone.
Horse latitude winds are dry, stable, and often calm areas that are found around 30 degrees latitude in both the Northern and Southern Hemispheres. These winds are typically associated with high-pressure systems and are characterized by weak or variable winds. The term "horse latitude" originated from the stories of Spanish sailors throwing their horses overboard when they became stranded in these calm zones during their voyages.
No, it can but it doesn't necessarily need a variable. I have no idea what the previous answer means. The earth spins on its axis. The spin axis provide the geographic north and south poles. On the other hand the earth's magnetism does not work like a bar magnet. Instead, the iron and cobalt core spins at a slightly faster rate than the rest of the earth. This sets up eddy electrical currents which creates magnetic fields. In the northern hemisphere, the magnetic fields join under Northern Canada.
An independent variable is the variable you can change in an experiment. On a graph, it's on the X-axis. A dependent variable is the result of changing the independent variable. It is literally dependent on it. The dependent variable goes on the Y-axis.
"Controlled Variable" or "Manipulated Variable"
the anwer is a variable( the thng that will change over time in the experiment
The ITCZ (inter-tropical convergence zone)
By using an electromagnet with a variable resister to finely-balance your spherometer's intrinsic, counter-clockwise torque--assuming that you are in the northern hemisphere. If you are in the Southern Hemisphere, then you'll simply need to reverse the polarity of your electromagnet.
The best answer I can give is they live almost exclusively in the Southern hemisphere. Beyond that is highly variable.
Horse latitude winds are dry, stable, and often calm areas that are found around 30 degrees latitude in both the Northern and Southern Hemispheres. These winds are typically associated with high-pressure systems and are characterized by weak or variable winds. The term "horse latitude" originated from the stories of Spanish sailors throwing their horses overboard when they became stranded in these calm zones during their voyages.
The generally accepted dates for New Zealand seasons are based on the reverse of those in the northern hemisphere, but these do not exactly correspond to the weather patterns in New Zealand, which are both more variable throughout the year and less extreme seasonally. It has been suggested by some that Australia and New Zealand each have their own weather patterns with 6 or so distinct seasons.Beginning dates for the standard 4 seasons in the southern hemisphere are:Autumn 1 MarchWinter 1 JuneSpring 1 SeptemberSummer 1 December
Depends on where you are. New Zealand has a very variable climate. It stretches from the sub tropical north to cold temperate in the south a distance of more than a thousand miles. There are mountains which never rise above freezing and very warm inland valleys in summer. One of these valleys in the south island has New Zealand's coldest and hottest temperatures. Excepting the mountains the highs in December range from 22 deg C to 35 deg C. Dropping to 12-24 at night. But even in December (our summer) cold storms can hit in the mountains and hill country.sometimes its really cold but usulley its warm
The brightest star in the sky, is our Sun. It is a star. After the Sun, Sirius is the next brightest star, or the brightest in the night sky.
When Earth is closest to the sun the Southern Hemisphere receives more of the sun's rays, making it hotter, or summer there, and winteri nthe north.
The seasons are popularly considered to start on different dates in different cultures based on astronomy and regional meteorology. When it is summer in the southern hemisphere it is winter in the northern hemisphere, and vice versa.Autumn (also known as Fall in North American English) is one of the four temperate seasons. Autumn marks the transition from summer into winter, usually in late March (southern hemisphere) or late September (northern hemisphere) when the arrival of night becomes noticeably earlier.In tropical regions this concept of seasons does not really apply. Summer is often reckoned to be the hottest time of the year, and winter the coolest. The year may be additionally divided into wet and dry seasons.From a purely astronomical viewpoint, the equinoxes and solstices would be the middle of the respective seasons, but a variable seasonal lag means that the meteorological start of the season, which is based on average temperature patterns, occurs several weeks later than the start of the astronomical season.Today, the meteorological reckoning of the seasons is used in Australia, Denmark and the former USSR; it is also used by many people in the United Kingdom. The definition based on equinoxes and solstices is more frequently used in the United States, where many regions have a continental climate with a temperature lag of about six weeks.In southern and southeast Asia, where the monsoon occurs, summer is more generally defined as lasting from March to May/early June, their warmest time of the year, ending with the onset of the monsoon rains. Winter begins after the monsoons, and it the coolest time of year. It lasts from November through January.Autumn is on September 23,2011
August is a Summer month, The first day of fall starts when the next soltice comes around which is usually on the 21 of the month. I cant remember when that is except March 21 is the first day of spring, June 21 is the first day of summer so Sept 21 must be fall
No, it can but it doesn't necessarily need a variable. I have no idea what the previous answer means. The earth spins on its axis. The spin axis provide the geographic north and south poles. On the other hand the earth's magnetism does not work like a bar magnet. Instead, the iron and cobalt core spins at a slightly faster rate than the rest of the earth. This sets up eddy electrical currents which creates magnetic fields. In the northern hemisphere, the magnetic fields join under Northern Canada.
variable is the variable that variable a variable into a variable. noOb