quadgram

This is a table of type quadgram and their frequencies. Use it to search & browse the list to learn more about your study carrel.

quadgram	frequency
the belt of rains	33
in relation to the	30
the surface of the	29
american journal of science	20
the temperature of the	20
the action of the	19
the character of the	19
of the united states	19
the course of the	18
surface of the earth	17
of the belt of	16
in the west indies	16
the direction of the	16
northern limit of the	14
at the same time	14
tropical belt of rains	14
is a sign of	13
east of the alleghanies	13
the northern limit of	13
on the western side	12
the body of the	12
the eastern portion of	12
the gulf of mexico	12
by the action of	12
the latter part of	12
the influence of the	12
seasons of the year	12
in the southern hemisphere	12
in the northern hemisphere	11
in the united states	11
in the form of	11
the western side of	11
a part of the	11
of the northern hemisphere	11
in the vicinity of	11
as we have seen	10
the elevation of the	10
a portion of the	10
western side of the	10
the western coast of	10
the equatorial rainy belt	10
the focus of precipitation	10
action of the sun	10
the situation of the	9
direction of the wind	9
the state of the	9
the mean of the	9
the bay of bengal	9
the same is true	9
the rays of the	9
jewel for the month	9
of the indian ocean	9
portion of the continent	8
under the belt of	8
portions of the earth	8
belt of rains is	8
the cape de verdes	8
we have seen that	8
in the character of	8
it will be seen	8
eastern portion of the	8
the rest of the	8
of the west indies	8
in the polar regions	8
at the surface of	8
the moisture of evaporation	8
to the green woods	8
belt of rains and	8
but it is not	8
the fact that the	8
of the rainy belt	8
a spinning we will	8
the phenomena of the	8
to account for the	8
limits of the trades	8
on the other hand	8
under the rainy belt	7
of the rocky mountains	7
state of the weather	7
philosophy of the weather	7
the fall of the	7
spinning we will go	7
the northern edge of	7
the united states weather	7
it is obvious that	7
course of the counter	7
the limits of the	7
united states weather bureau	7
portion of the storm	7
when the sun is	7
the level of the	7
for the purpose of	7
latter part of the	7
limit of the n	7
the difference in the	7
author of many books	7
according to the season	7
the interior of the	7
rays of the sun	7
side of the great	7
from north to south	7
in the course of	7
on the th of	7
in the same latitude	7
the range of the	7
phenomena of the weather	7
the trade and the	7
cut your nails on	7
and a spinning we	7
will be seen that	7
the earth and the	7
body of the storm	7
when the moon is	7
it is a sign	7
coast of south america	6
the mentor reading course	6
in the same manner	6
the tables of dr	6
the western portion of	6
far as i have	6
it is difficult to	6
level of the sea	6
between it and the	6
in the summer months	6
of the gulf stream	6
during the dry season	6
in connection with the	6
the manner in which	6
the middle of the	6
for the first time	6
at the rate of	6
of the new york	6
of the atmospheric machinery	6
the height of the	6
in the mentor reading	6
at all seasons of	6
of the storm cloud	6
as well as the	6
condensation in the trade	6
of the cape de	6
of the equatorial rainy	6
the earth to the	6
your nails on a	6
does not seem to	6
one of the most	6
the eastern side of	6
the formation of cloud	6
the head of the	6
in the center of	6
they who wash on	6
so far as i	6
in the american journal	6
the center of the	6
the close of the	6
it and the earth	6
from the earth to	6
in obedience to the	6
this class of storms	6
different portions of the	6
the cape de verde	6
western portion of the	6
is supposed to be	6
the american journal of	6
the philosophy of the	6
all seasons of the	6
and author of many	6
the th of september	6
it is not a	6
between the parallels of	6
of the surface winds	6
the reciprocal action between	5
it is unlucky to	5
the line of perpetual	5
of the nature of	5
between the earth and	5
and the indian ocean	5
the belt of precipitation	5
gives us the following	5
there is an old	5
the lines of magnetic	5
to one hundred and	5
hundred and fifty miles	5
northern edge of the	5
during the northern transit	5
the southern edge of	5
of the bay of	5
north and south of	5
is true of the	5
depression of the barometer	5
the heat of the	5
the form of a	5
between the trade and	5
the west and north	5
part of the storm	5
before the week is	5
in upon the land	5
the western edge of	5
in a similar manner	5
western coast of south	5
southern line of the	5
of the air is	5
transit north and south	5
to the north of	5
the passage of the	5
on the surface of	5
state of the atmosphere	5
on the d of	5
the west coast of	5
to the action of	5
the top of the	5
spots upon the sun	5
the southern line of	5
range of the thermometer	5
the path of the	5
from south to north	5
the vicinity of new	5
same is true of	5
who wash on a	5
as soon as the	5
to which we have	5
the zone of extra	5
the transit of the	5
line of perpetual snow	5
have seen that the	5
within two or three	5
and in relation to	5
the wind from the	5
influence of the sun	5
as we shall see	5
to the fact that	5
the progress of the	5
line of magnetic intensity	5
of the most important	5
cape de verde islands	5
there is a tendency	5
produced by the action	5
the great region of	5
the waters of the	5
of heat and cold	5
the magnitude of the	5
different seasons of the	5
in the first place	5
when there is no	5
of the equatorial belt	5
on the opposite side	5
portions of the storm	5
in relation to this	5
of the great oceans	5
from the south atlantic	5
is the result of	5
the base of the	5
the fall of rain	5
to a considerable extent	5
to show that the	5
temperature of the air	5
the valley of the	5
the direct action of	4
wind from the s	4
of the air at	4
of the surface atmosphere	4
the sun is at	4
in the indian ocean	4
which falls upon the	4
within the arctic circle	4
eastern portions of the	4
the moon is on	4
magnetic intensity of the	4
when the wind blows	4
transit of the atmospheric	4
great region of expansion	4
on either side of	4
central belt of rains	4
within influential distance of	4
the southern limit of	4
the presence of the	4
the central belt of	4
the truth of the	4
the week is out	4
in the south atlantic	4
the formation of cumuli	4
to a higher elevation	4
north of the tropics	4
the sky is red	4
the theory of mr	4
to the character of	4
is shown by the	4
trades of the atlantic	4
on the st of	4
the secretary of defense	4
of the wind at	4
and there is no	4
at miles an hour	4
is said to be	4
fall of the barometer	4
as far as the	4
currents of the atmosphere	4
character of the surface	4
and south of the	4
author of various books	4
the belt of inter	4
close of the storm	4
as it is termed	4
in proportion to its	4
either side of the	4
the surface atmosphere from	4
way to a higher	4
the th of august	4
to the north and	4
and on the th	4
to the east of	4
under a vertical sun	4
to believe that the	4
woods we will go	4
and force of the	4
of the weather bureau	4
in consequence of the	4
from the surface of	4
the existence of a	4
but it is a	4
this part of the	4
and character of the	4
at the mouth of	4
any portion of the	4
on the same day	4
of an approaching storm	4
at the northern limit	4
direct action of the	4
in the same direction	4
part of the day	4
the burning plains of	4
in the latitude of	4
that part of the	4
over the surface of	4
shall recur to this	4
there is not a	4
and north of the	4
on the western coast	4
the existence of the	4
of the parallel of	4
is a tendency to	4
the monsoons of the	4
on the east of	4
the south of the	4
action in the counter	4
in the absence of	4
over the united states	4
the typhoons of the	4
if it were not	4
in july and august	4
pressure of the air	4
of the sun in	4
body of the atmosphere	4
a medley of weather	4
the same manner as	4
on the eastern side	4
moon is on the	4
in relation to which	4
the eastern part of	4
of this class of	4
make room for may	4
lines of magnetic force	4
monsoons of the indian	4
wind from the east	4
extended stratum of stratus	4
a change of the	4
all the phenomena of	4
of the focus of	4
the changes of the	4
theory in relation to	4
a greater or less	4
that portion of the	4
is by no means	4
rainy and dry season	4
edge of the storm	4
and author of various	4
by reason of the	4
influence of the earth	4
other things being equal	4
southern limit of the	4
of the mentor association	4
in the upper regions	4
sun is at the	4
the law of curvature	4
during the rainy season	4
the green woods we	4
in opposition to the	4
north of the parallel	4
the result of the	4
the latter half of	4
us the following table	4
of the atmosphere are	4
in the month of	4
the region of the	4
in the day time	4
of america in pictures	4
to the region between	4
the location of the	4
green woods we will	4
situation of the focus	4
with the aid of	4
the ocean and the	4
state of things is	4
the irregular action of	4
earth and the counter	4
surface of the ocean	4
off to the eastward	4
southern edge of the	4
the weight of the	4
of the british association	4
may be seen in	4
in the order n	4
where the air is	4
limit of the equatorial	4
of the gulf of	4
months of the year	4
the last of the	4
day be fair and	4
i have known it	4
the mouth of the	4
the magnetic intensity is	4
of the trades and	4
part of the continent	4
finds its way to	4
influence upon the weather	4
as we have already	4
action of terrestrial magnetism	4
elevation of the counter	4
above the level of	4
its way to a	4
the volume of the	4
vicinity of new york	4
to the influence of	4
focus of precipitation in	4
from the action of	4
the east of the	4
the first of may	4
in the interior of	4
the calms of cancer	4
medley of weather lore	4
of the isothermal lines	4
the same state of	4
i have already said	4
the story of the	4
easterly wind and scud	4
it should be remembered	4
story of america in	4
sea breeze set in	3
portions of the country	3
that there is not	3
polar belts of condensation	3
a distance of from	3
the northern and southern	3
and when it is	3
when the sun shines	3
its course of progression	3
rainy and dry seasons	3
of moisture in the	3
to the south of	3
the wind of the	3
state of the trade	3
in proportion to the	3
the countenance of the	3
of the storm to	3
that there is an	3
the line of magnetic	3
on the south of	3
of the character of	3
when the atmosphere is	3
followed by the n	3
mentor reading course the	3
the first time you	3
all over the country	3
forty to one hundred	3
in the direction of	3
the difference of temperature	3
the eastern portions of	3
of the influence of	3
during the latter half	3
phenomena of the atmosphere	3
for the benefit of	3
to snow or rain	3
as far north as	3
have been able to	3
by the existence of	3
the coast to the	3
the period of the	3
shepherd heaves a sigh	3
pass through each other	3
local moisture of evaporation	3
the eastern united states	3
and currents of the	3
a stream of fog	3
at the close of	3
so far as we	3
they show an increase	3
of the coast to	3
the extension of the	3
elevation of the isothermal	3
there is a vast	3
base of the rocky	3
of the calms of	3
of the approaching storm	3
the rate of twenty	3
any place on the	3
different forms of cirro	3
trade near the earth	3
at the height of	3
on the north side	3
surface atmosphere from the	3
there has been no	3
in the opposite direction	3
a state of things	3
in the foregoing extract	3
the trade near the	3
that it is not	3
trade and the earth	3
very fine and clear	3
with the exception of	3
during the latter part	3
middle and latter part	3
no weather is ill	3
journal of science and	3
of north america and	3
journal of science for	3
that which falls upon	3
the spots upon the	3
be seen that the	3
we shall see hereafter	3
edge of an approaching	3
the surface atmosphere of	3
hollow winds begin to	3
with reference to the	3
in the midst of	3
the intensity of the	3
which overlies the storm	3
as we have said	3
at a time when	3
to two thousand miles	3
line of no variation	3
the circular currents of	3
of the whole machinery	3
in storms and showers	3
an extended stratum of	3
will be found in	3
to the west and	3
with which we are	3
and the focus of	3
manner in which it	3
in like a lion	3
other portions of the	3
north of the northern	3
if the storm is	3
the southern portion of	3
nothing must be drank	3
after the sea breeze	3
night the sun went	3
northern portions of south	3
of the mountain ranges	3
a belt of showers	3
quite to the summit	3
as it passes over	3
the land and the	3
on the west coast	3
and in the rapid	3
portions of south america	3
storms originate in it	3
numbers of the mentor	3
time will come when	3
but owing to the	3
the evening of the	3
risen quite to the	3
character of the seasons	3
to the difference in	3
at the base of	3
for the time being	3
to the line of	3
if apples bloom in	3
should be remembered that	3
eastern side of the	3
side of the gale	3
south of the equator	3
part of the month	3
of the northern limit	3
in the body of	3
boding shepherd heaves a	3
from the fact that	3
may be found in	3
the contiguity of the	3
of the lines of	3
winds begin to blow	3
of the atmosphere is	3
by the fact that	3
to the contiguity of	3
will be dear all	3
irregular action of the	3
three or four days	3
westward to the eastward	3
the place where the	3
the sudden expansion of	3
from a westerly point	3
from the east or	3
five hundred miles in	3
on the south side	3
that there was an	3
different state of things	3
as indicated by the	3
portion of the northern	3
did he do it	3
in the rapid eddy	3
i have seen them	3
center of the storm	3
difference in the character	3
such a state of	3
from right to left	3
that a storm is	3
hour of the day	3
after the passage of	3
before it reaches the	3
interior of the country	3
power of attracting the	3
the extent of the	3
as all men do	3
been attributed to the	3
from thence to the	3
is a part of	3
and the west indies	3
as soon as they	3
bank of haze in	3
portions of the cloud	3
central portions of the	3
the most important of	3
all things in tune	3
all parts of the	3
in the light of	3
during the months of	3
northern transit of the	3
the first new moon	3
if there be any	3
show that it is	3
two or more currents	3
on the pacific coast	3
by reason of its	3
to the course of	3
investigated by professor loomis	3
the indian summer of	3
oak before the ash	3
of the solar rays	3
the immediate neighborhood of	3
the middle of june	3
rest of the world	3
the local moisture of	3
there is a tradition	3
the surface atmosphere is	3
one or the other	3
from the west and	3
over the whole country	3
a swarm of bees	3
the volume of counter	3
when it was the	3
of the magnetic poles	3
very near the earth	3
indian summer of autumn	3
and that it is	3
the desert of sahara	3
with or without rain	3
of that which falls	3
reliance can be placed	3
north of its southern	3
swarm of bees in	3
attempt to account for	3
the nearer to twelve	3
return of the belt	3
it is a mistake	3
in accordance with his	3
in the summer season	3
the greater part of	3
the moon in the	3
from the middle of	3
the th of february	3
to the southward of	3
same state of things	3
the rainless portions of	3
feet above the level	3
east of the mountains	3
is newly risen quite	3
in april and may	3
which takes place between	3
the rise of the	3
primary action in the	3
can be placed upon	3
the west india islands	3
to the west indies	3
is explained by the	3
magnitude of the variations	3
but it may be	3
of the philosophy of	3
from positive to negative	3
the theory of rarefaction	3
of the concentrated trade	3
as they approach the	3
latter half of the	3
be fair and clear	3
the wind is from	3
on the first of	3
coast of north america	3
the west indies and	3
and at other times	3
coming into each other	3
up as far as	3
of which we have	3
to which we shall	3
lines of no variation	3
for three or four	3
in the present state	3
the under surface of	3
been able to discover	3
accordance with his theory	3
and the temperature of	3
the sea breeze set	3
of the storm passed	3
an earthquake and a	3
the place of the	3
the boding shepherd heaves	3
direction and force of	3
in the evening the	3
i have been able	3
on the verge of	3
the advance condensation of	3
the northern portions of	3
the supposed vortex of	3
the south atlantic and	3
i shall recur to	3
the changes in the	3
the pacific coast of	3
the rapid eddy plays	3
the belt of extra	3
height of the barometer	3
and it is not	3
the region of extra	3
action between the earth	3
side of the island	3
owing to the fact	3
in no other way	3
eastern edge of an	3
of greatest magnetic intensity	3
the diffusion of heat	3
action between it and	3
reliance may be placed	3
such a stream of	3
may be well to	3
countenance of the sky	3
one to two thousand	3
the differences in the	3
but i can not	3
the gathering of the	3
went pale to bed	3
in the spring and	3
passed off to the	3
it may be well	3
the extreme limits of	3
it will not do	3
summit of his prison	3
the present state of	3
the distant hills are	3
of the wind is	3
on the th it	3
one hundred and fifty	3
it seems to be	3
is increased by the	3
at the time of	3
calms and baffling winds	3
the oak before the	3
last night the sun	3
if there be a	3
during the night and	3
the st of february	3
in relation to them	3
belt of daily rains	3
the eastern edge of	3
the return of the	3
over the entire hemisphere	3
in our own country	3
of rains and calms	3
sudden expansion of the	3
which finds its way	3
this power of attracting	3
the cuckoo sings in	3
we are enabled to	3
the th of the	3
below the cape de	3
critic of the new	3
given out during condensation	3
they who bathe in	3
be seen in the	3
the north side of	3
trending of the coast	3
action which takes place	3
are on the rack	3
where there is no	3
in a few instances	3
at the same angle	3
when it has been	3
is obvious that the	3
for the most part	3
off her left shoe	3
of the winds in	3
the westward to the	3
keys of the year	3
over the area of	3
the east or south	3
weather and folk lore	3
is diffused over the	3
where the magnetic intensity	3
the keys of the	3
the face of the	3
is found in the	3
rainbow spans the sky	3
america and southern mexico	3
the nature of the	3
which we have alluded	3
so that it may	3
for the rest of	3
to which i have	3
the inducing and attracting	3
within the range of	3
the belt of calms	3
the machinery of distribution	3
of the continent of	3
i have said that	3
there is no storm	3
at the line of	3
the commencement of the	3
the belt of condensation	3
the wind blows from	3
carried in the pocket	3
is one of the	3
the space from which	3
reciprocal action which takes	3
one third of the	3
and the reciprocal action	3
this is the result	3
the water and air	3
from one to two	3
newly risen quite to	3
in advance of the	3
from the westward to	3
part of the subject	3
currents of an opposite	3
on the top of	3
toward the close of	3
the northern transit of	3
and there is a	3
of the southern line	3
part of the country	3
deprived of its moisture	3
the time will come	3
of the reciprocal action	3
which is within the	3
by the course of	3
by the formation of	3
and the burning plains	3
when the belt of	3
is such as to	3
the variations in the	3
by the increase of	3
early part of the	3
if it does not	3
the sun went pale	3
it were not for	3
the borders of the	3
it is not the	3
of five hundred miles	3
north of the cape	3
th of the month	3
for two or three	3
as i have observed	3
of the china sea	3
of showers and storms	3
increase of magnetic intensity	3
the direction and force	3
reason to believe that	3
from a daguerreotype view	3
attracts the surface atmosphere	3
to the eastward of	3
were not for the	3
a state of the	3
reciprocal action between the	3
the storm clouds are	3
of the storm is	3
the middle and latter	3
chance to snow or	3
of the great region	3
the storm of professor	3
when this is so	3
it is not only	3
trades of the pacific	3
central america and southern	3
in the immediate neighborhood	3
a day or two	3
character of the clouds	3
and folk lore of	3
the more central portions	3
limit of the s	3
the production of the	3
of the continent in	3
the walls are damp	3
from one side of	3
the soot falls down	3
the various forms of	3
their supply of moisture	3
to the region of	3
wind of the south	3
the electricity of the	3
volume of the trades	3
of the sun upon	3
more central portions of	3
it is by no	3
the summit of his	3
of science and art	3
and phenomena of the	3
is unlucky to bring	3
but i am not	3
portion of the atlantic	3
their connection with the	3
in contact with the	3
the part of the	3
storm of professor loomis	3
the north of the	3
in regard to the	3
the following table of	3
under the zone of	3
relation to the monsoons	3
the movement of the	3
an extension of the	3
a different state of	3
typhoons of the china	3
of the difference in	3
extreme limits of the	3
portion of the earth	3
by the middle of	3
a knowledge of the	3
the poles of the	3
of attracting the surface	3
the time of the	3
rainless portions of the	3
the difference between the	3
appear in the sequel	3
it is to be	3
of the meridian of	3
the different forms of	3
portion of the pacific	3
there is no such	3
two or three miles	3
to look at the	3
some point between s	3
i have never seen	3
they are produced by	3
at different seasons of	3
rise of the barometer	3
joints are on the	3
in accordance with the	3
sun went pale to	3
to forty degrees of	3
evaporation is going on	3
blue sky and detached	3
this belt of rains	3
from some point between	3
is owing to the	3
and in connection with	3
changes of the weather	3
to a consideration of	3
a health to the	3
influential distance of the	3
with the difference in	3
the clouds and currents	3
then will be dear	3
of the currents of	3
the surface winds of	3
by the mentor association	3
elevation of the barometer	3
the year is the	3
of the concentrated counter	3
in autumn and winter	3
will appear in the	3
points of the compass	3
course of the storm	3
front of the storm	3
is placed in the	3
too far south to	3
a sign of a	3
is blowing from the	3
a rainbow spans the	3
of the magnetic currents	3
to the extent of	3
in the middle of	3
above the mean in	3
the hollow winds begin	3
the appearance of a	3
ascending to the region	3
passing over to the	3
out over the atlantic	3
the wind was blowing	3
which are accompanied with	3
condensation at the west	3
upon the same parallels	3
winds north of the	3
we shall find that	3
the conquest of the	3
at the present time	3
how are storms produced	3
in may and june	3
very soon after the	3
the line of extra	3
where intensity is greatest	3
to the summit of	3
the position of the	3
in summer and autumn	3
on the leeward side	3
with the formation of	3
the early part of	3
near the earth is	2
ill does the leaf	2
the increase of magnetic	2
setting in of a	2
and the scud running	2
to urge my perilous	2
the result of their	2
from which the rain	2
the observatory on monte	2
meteorological station in the	2
five miles an hour	2
eastern edge to the	2
observer must be careful	2
of the current of	2
supposed to be conducted	2
the seasons have a	2
result of his observations	2
that the focus of	2
the bay of panama	2
northern extension of the	2
rainy belt up to	2
lore of peterborough and	2
by the passing storm	2
and dying away at	2
but i shall recur	2
front of a house	2
luck into a house	2
at the tropic of	2
it is also a	2
once when it is	2
cape of good hope	2
the storm is coming	2
meads with eager bite	2
the fairest or foulest	2
heated air along the	2
and the line of	2
fear no coming rain	2
in the lamp crackles	2
parts of the country	2
to some point between	2
the analogy between this	2
the number of the	2
that the latter are	2
is within the region	2
or a succession of	2
or south of the	2
portion of the n	2
advance portion of the	2
to smell wild thyme	2
in the fall of	2
cloud of the storm	2
toward an approaching storm	2
the cape of good	2
heat supposed to be	2
speaking ill of you	2
an excuse for not	2
the needle every where	2
or lines of force	2
sun did not set	2
will it be before	2
large volume of n	2
as the western edge	2
in the region of	2
it is not in	2
the temperature was above	2
limit is carried up	2
one month is past	2
or to the east	2
north of the rainless	2
shore of long island	2
a kindly good january	2
are produced by the	2
the earth which the	2
i met queen spring	2
all men do think	2
place between it and	2
weather is ill if	2
the make of the	2
a tuft of evening	2
to be relied upon	2
and all the phenomena	2
again until all the	2
reflect the rays of	2
it is found in	2
our portion of the	2
the general or local	2
if march comes in	2
hundred million dollars a	2
haul to the s	2
from the indian ocean	2
the wind gets around	2
a wet good friday	2
heat of the day	2
of rains and the	2
of the winds at	2
the spring and autumn	2
shows one phase of	2
wind and the rain	2
drop flurries of snow	2
and the storm is	2
an extreme northern transit	2
burning plains of central	2
deserts of cobi and	2
in the same latitudes	2
they may be seen	2
much lightning in south	2
when the white pinks	2
in a majority of	2
in the phenomena of	2
difference in the seasons	2
the air at the	2
air is cold and	2
i can not answer	2
sportive feathers circle on	2
is occasioned by the	2
portion of north america	2
just conception of the	2
when the sloe tree	2
in spring and summer	2
wild with the winds	2
the point from which	2
distant hills are looking	2
in one or two	2
harry bettis did not	2
to the same cause	2
excess of negative electricity	2
the usual course of	2
the sun shines on	2
the monsoons are blowing	2
am well aware that	2
and the wind was	2
for the space of	2
on the same parallel	2
dense enough to drop	2
whether hot or cold	2
the normal conditions of	2
all this is the	2
air of the monsoon	2
the great oceanic currents	2
the negative electricity of	2
edge of the belt	2
of magnetic intensity and	2
the rays of a	2
the electricity is disturbed	2
the air near the	2
differ greatly from one	2
rain does not fall	2
in the trade and	2
will show that the	2
a dingy suit is	2
near the line of	2
is very certain to	2
way through each other	2
for the return of	2
it has been found	2
to the south and	2
from the different sides	2
north or south of	2
in spring and autumn	2
is represented in the	2
in the same way	2
a fog is a	2
distinctly from the east	2
on the way to	2
half of the decade	2
immediate neighborhood of active	2
who shears his sheep	2
the desert of cobi	2
of this belt of	2
are sweet in the	2
the front of an	2
on its eastern shores	2
an increase of the	2
some portion of the	2
a line of heavy	2
with or without a	2
with a view to	2
is not as great	2
sufficient accuracy for illustration	2
i have termed them	2
in different portions of	2
to the third girl	2
agency in producing the	2
how strong soever the	2
makes a fat churchyard	2
nimbly catch the incautious	2
one of the best	2
over the left shoulder	2
on the malabar coast	2
it may seem to	2
reciprocal action between it	2
lighting up in the	2
be the best bird	2
some of the most	2
sides of the island	2
magazine writer and author	2
point from which the	2
region of atmospheric expansion	2
wildly rage with squalls	2
greater part of the	2
northern mexico and the	2
must be drank before	2
the banks of newfoundland	2
region of the trade	2
from chimneys right ascends	2
of the body of	2
it to have been	2
of the surface trades	2
the mean temperature for	2
fell below the mean	2
the side of the	2
air is supposed to	2
and to her bed	2
feathers of the willow	2
at the th parallel	2
an eastern progression of	2
and so it is	2
and portions of it	2
mouth of the huallaga	2
if we set a	2
harvest shall not cease	2
the thermometer stood at	2
condensation is sufficiently dense	2
in relation to each	2
is covered by the	2
the sun does not	2
the barn will fill	2
diffused over the earth	2
the feathers of the	2
both sides of the	2
whole body of the	2
lightning and what causes	2
it is made to	2
measure of the air	2
by the belt of	2
to carry it over	2
the good old year	2
one phase of them	2
and over to the	2
clouds and currents of	2
doubtless in all cases	2
latitude with the variations	2
squalid toad was seen	2
to my notice since	2
the aid of a	2
come to speak of	2
was followed by a	2
falls upon the alleghanies	2
the table lands of	2
in the earlier part	2
the influence of magnetism	2
that they do so	2
south and central america	2
the reign of heat	2
the proportion of the	2
and of surface condensation	2
whatever it may be	2
on this subject i	2
of the trade winds	2
up from the south	2
is connected with the	2
roof of a house	2
primary influence of the	2
the chairs and tables	2
their storms in a	2
the sun upon the	2
a stunt like that	2
part of the trade	2
and horizontal and vertical	2
the annexed cut shows	2
not even wireless communication	2
and i have known	2
but one maximum and	2
coming out of the	2
and whence thou mayst	2
position is shown by	2
of the diurnal motion	2
water like the ocean	2
for a longer or	2
when the rainy belt	2
of the boiling water	2
scent of the rose	2
the gentle easterly breeze	2
winds of the west	2
have been but two	2
and in the s	2
rage with squalls and	2
with squalls and driving	2
all that thence successive	2
not effect changes at	2
the first of march	2
forms of cirrus and	2
one thousand to fifteen	2
belie the constant sun	2
few hundred miles of	2
and on the south	2
may be said that	2
as far as i	2
in the interior and	2
posts of the united	2
an incident of the	2
the lamp crackles the	2
the storm is not	2
the south of us	2
to draw the s	2
and south of quebec	2
not seem to have	2
have already said that	2
change of the weather	2
of peterborough and district	2
the reciprocal action which	2
morning of the th	2
northern boundary of the	2
for a stunt like	2
to understand the precise	2
such a knowledge of	2
storm after the wind	2
is nearly proportional to	2
th december to th	2
it does not exist	2
portions of the pacific	2
hauling to the south	2
and may are the	2
the belt of the	2
at the top of	2
the tops of the	2
in the bay of	2
be put off to	2
outside of the tropics	2
wind was blowing from	2
oft wander on his	2
of was owing to	2
the following five years	2
up to the region	2
at right angles to	2
explain all the phenomena	2
and one or two	2
cheek burning someone is	2
in different countries of	2
in either case the	2
who knows what i	2
when a storm is	2
all the year is	2
fell to the depth	2
he looked at johnny	2
belt of rains from	2
one class of storms	2
comes in the sweet	2
more distinctly from the	2
very much in proportion	2
its eastern edge to	2
and throw it over	2
wind gets around to	2
run off at the	2
may know it from	2
health unto our master	2
mow me down the	2
passed the limits of	2
it chance to snow	2
the leaf defend the	2
excuse for not accepting	2
of the weather elsewhere	2
when there are three	2
the east in the	2
able to prove it	2
he who supposes that	2
march does from april	2
showery climate of england	2
worse for it all	2
edge of our concentrated	2
is north of us	2
the exploration of the	2
of one thousand miles	2
and functions of the	2
appearance of the sky	2
functions of the counter	2
the character of a	2
on the grass and	2
airs will fan the	2
the barometer in the	2
different countries of equal	2
condensation of a storm	2
and if it is	2
it is evident that	2
will find in the	2
redfield and lieutenant maury	2
very well can both	2
the reader is desired	2
with such wonderful regularity	2
path of the tornado	2
middle of june to	2
the reverse is true	2
we know that these	2
as may be seen	2
are more frequent in	2
if the ruddy blaze	2
state of things exists	2
glimmers obnoxious to her	2
has but one maximum	2
inconsistent with the theory	2
the barometer rises rapidly	2
the belief that the	2
the warm air of	2
from buenos aires to	2
waters of the indian	2
any given portion of	2
felt the piercing ball	2
where the wind is	2
the same parallels of	2
of temperature does not	2
the heated air along	2
number of days in	2
altitude of the sun	2
the observations of professor	2
then all will wildly	2
and for the whole	2
the spots and magnetic	2
in the leeward gulf	2
rain at all seasons	2
bank in the west	2
our jaunt must be	2
on a line with	2
table lands of thibet	2
trade which curves over	2
the regular action of	2
the clouds of the	2
if the sage tree	2
when the spots were	2
the busy flies disturb	2
for the next three	2
more glimmers obnoxious to	2
will soon be able	2
a type of all	2
currents of air which	2
moon and the weather	2
what is true of	2
by means of the	2
than in any other	2
in the shape of	2
or seem precipitate to	2
the varying moon that	2
our greater magnetic intensity	2
an end of the	2
a portion of it	2
the wind may blow	2
defend the mellowing grape	2
of southern and central	2
hills are looking nigh	2
be covered by the	2
continued depression of the	2
over the desert of	2
storm investigated by professor	2
love on a day	2
the spring is coming	2
now set for thy	2
by the observations of	2
severity of the cold	2
result of their action	2
the following cut and	2
earth varies in the	2
sweet is the rose	2
to a greater or	2
we know of it	2
hundred miles in diameter	2
is taken up there	2
from the observations of	2
a large volume of	2
equatorial rainy belt does	2
run into the sea	2
clouds to mount the	2
wind may blow from	2
of the class of	2
fairest or foulest day	2
about the middle of	2
form near the earth	2
and in the same	2
there is an intimate	2
facts in relation to	2
and into the rainy	2
for the same reason	2
in the neighborhood of	2
first in the north	2
when the corn begins	2
mighty mountains pour a	2
the northern extension of	2
on this day as	2
february fill the ditch	2
of the sun and	2
that of the earth	2
when the barometer was	2
at dusk the squalid	2
the first and second	2
two in the afternoon	2
the distribution of heat	2
off the malabar coast	2
article in the american	2
shall have occasion to	2
heat of the sun	2
the earlier part of	2
west of the magnetic	2
there is not such	2
have seen them in	2
perhaps it is not	2
that occur in the	2
hurricanes of the west	2
are incidents of the	2
the presence or absence	2
far south to be	2
rise and create a	2
the opposite is true	2
of primary or magneto	2
on the west of	2
thorney the flower of	2
i have seen the	2
frog has lost his	2
feathers circle on the	2
meteorologists of this country	2
all over the globe	2
precise character of the	2
bearing upon the question	2
the ascensive force of	2
influence of the moon	2
if the condensation is	2
near the lateral confines	2
considerable portion of the	2
and in a dingy	2
our storms originate in	2
in a more marked	2
the wind at the	2
and look at oats	2
of the day and	2
light of a correct	2
no means certain that	2
there is never a	2
cut thistles in may	2
wind of western europe	2
had a garland of	2
the most inconsiderable portion	2
to do with the	2
then wades through clouds	2
to the eastward and	2
april and may are	2
of vapor in the	2
on grass to feast	2
sun set in a	2
her bed untimely send	2
who rings the best	2
the volcanic series of	2
clearing wind shall waft	2
that the years differ	2
to illustrate this further	2
far along the beach	2
above the machinery of	2
on account of the	2
thousand miles or more	2
light chaff and leaflets	2
with his head in	2
of that which has	2
observatory on monte rosa	2
that there has been	2
seasons of different years	2
law of curvature and	2
are upon the same	2
and in a few	2
discovery of the truth	2
on the eastern part	2
until they reach the	2
phases of the weather	2
travel north and south	2
to be observed that	2
ascent to a colder	2
of some of the	2
an old english proverb	2
bell is still rung	2
that the easterly wind	2
will sing another tune	2
present state of science	2
i copy from a	2
upon the western coast	2
above the earth varies	2
at the several stations	2
they have the wind	2
curving to the east	2
of curvature and progress	2
corresponding pole in the	2
of rain or snow	2
when the new moon	2
passed over to the	2
on that side of	2
of the dry belt	2
monsoons are found in	2
the rosy month of	2
vapor which finds its	2
of the same wind	2
how are they produced	2
the leeward gulf dash	2
and it is a	2
it fell to the	2
lightly through the sky	2
rays through the dense	2
of rain and snow	2
that the spots exert	2
sufficient to produce such	2
in the fall and	2
hurricanes begin from the	2
the excess of heat	2
and the result was	2
greatest where intensity is	2
the rainy belt upon	2
takes place in gales	2
do for the forces	2
is not that of	2
the highest temperature found	2
fog is a cloud	2
in height at its	2
the mentor association is	2
how the chairs and	2
in the same place	2
approach more nearly the	2
roof the plenteous hail	2
beach rolls the deep	2
in the middle and	2
passing off to the	2
make a country excursion	2
the squalid toad was	2
be cool and moist	2
for a like cause	2
the lines of equal	2
on a large scale	2
when sinks his tranquil	2
or two hundred miles	2
the ocean and lowlands	2
for in the west	2
a saying that if	2
along the beach rolls	2
of a fair day	2
it may be observed	2
in a level country	2
the condensation in the	2
from their cobwebs creep	2
trades upon the western	2
for a few weeks	2
we have seen in	2
upon the atlantic coast	2
usual course of this	2
opposite and corresponding pole	2
of the latter is	2
the west of the	2
the following are the	2
heat and moisture are	2
of the local moisture	2
miles of the earth	2
altered in his taste	2
line of the extra	2
the same latitude with	2
quantity of rain which	2
whispering grove betrays the	2
known magazine writer and	2
portion of the surface	2
not accepting the invitation	2
the character of storms	2
the light of the	2
to the west over	2
blow in a direction	2
intensity is nearly proportional	2
the month of august	2
go and look at	2
an average of about	2
and rain or snow	2
mountains pour a harsh	2
it may be said	2
one side of the	2
take place in the	2
the thermometer for the	2
the tranquil night will	2
western portion of our	2
their way through each	2
toil the tangled fleece	2
trade and the barometer	2
see an article by	2
one by professor loomis	2
though now no more	2
and it has been	2
flies disturb the kine	2
and does not deserve	2
of the day is	2
and their connection with	2
it will be found	2
the sky a perfect	2
the wind be still	2
become familiar with the	2
if the robin sings	2
north of the southern	2
in the belt of	2
projection of the lines	2
of calms and rains	2
greatly from one mile	2
storm condensation of the	2
it must be remembered	2
for the latter part	2
galleries of the world	2
local differences and peculiarities	2
an increase of activity	2
looked for in the	2
during the same season	2
magnetism and its associated	2
also supposed to be	2
our storms clear off	2
the intense magnetic area	2
from th december to	2
induced and attracted by	2
off over the atlantic	2
the nights grow cooler	2
does the leaf defend	2
forty degrees of latitude	2
west if issuing on	2
to work for the	2
if the grass grows	2
side is a field	2
between cloud and earth	2
in the old world	2
from which our rivers	2
read in the light	2
to listen to the	2
is on the wane	2
central office of the	2
temperature of the counter	2
drawing by the rev	2
as extensive as the	2
a longer or shorter	2
sawtry by the way	2
in march is good	2
return in the form	2
of a rotary gale	2
sky and detached clouds	2
do not want change	2
than upon the atlantic	2
supposed to be derived	2
in spring and fall	2
character of the phenomena	2
a great favourite and	2
the leeke is white	2
or there may be	2
over to the opposite	2
when they set in	2
or might have seen	2
one or two hundred	2
the next in order	2
edge of the extra	2
what we know of	2
contact with the earth	2
a more or less	2
no more glimmers obnoxious	2
and their supply of	2
and at that still	2
if it chance to	2
wind and current charts	2
nine times to the	2
portion of the trade	2
why this is so	2
winds the dust obeys	2
not have a vortex	2
seems to have been	2
the north of us	2
fourth night her lucid	2
over to the east	2
in october and beginning	2
reproduced in the indian	2
relation to which we	2
forty cases of rain	2
look again in june	2
can not be sustained	2
what clearing wind shall	2
before and during storms	2
it is said to	2
worn on that day	2
the west to the	2
of the atmosphere by	2
the ash before the	2
side of the rainy	2
by the direct action	2
action of the currents	2
the stars shine forth	2
had been no rain	2
from warm to cold	2
intense portions of the	2
off to the east	2
clouds of the storm	2
of the th of	2
they seem to be	2
of the fact that	2
not dense enough to	2
the upper or counter	2
about the time when	2
which curves over the	2
focus of precipitation is	2
a heavy fall of	2
the lower surface of	2
region of the n	2
it is otherwise in	2
by no means certain	2
or belt of showers	2
you may see the	2
western edge of our	2
and over the sea	2
be well to look	2
fingered rays through the	2
above the surface of	2
all hurricanes begin from	2
the track is often	2
the most distinguished meteorologist	2
and in certain localities	2
continue in that quarter	2
the storm condensation of	2
in the south orkneys	2
a most favored region	2
from the same quarter	2
late in the afternoon	2
the boundary line between	2
difficult to determine what	2
corns with shooting pains	2
when a cock drinks	2
at the commencement of	2
it is about to	2
it may be of	2
all through the sultry	2
shall find that the	2
those which have been	2
sudden and considerable rise	2
the indian ocean and	2
while the storm clouds	2
dying away at nightfall	2
which flow from the	2
winds than are found	2
the beginning of the	2
by the investigations of	2
in the production of	2
the page of nature	2
is to be observed	2
hundred miles of the	2
of the barbary states	2
been observed by others	2
to rise and create	2
a southern lateral extension	2
and the air over	2
his history of jamaica	2
the sun is vertical	2
and it will fall	2
night her lucid disk	2
republished in the american	2
heated in its interior	2
in the latter part	2
of the air and	2
a most beneficent provision	2
south of the cape	2
know the best season	2
betrays the gathering elemental	2
and curve in upon	2
in which they form	2
hundred miles or more	2
in most of the	2
the rain fell in	2
some portions of the	2
month of the year	2
come from the south	2
of the primary condensation	2
and the sun shines	2
her lucid disk define	2
on the east and	2
hours of the day	2
and it is said	2
within the region of	2
by the th of	2
over again until all	2
from those of other	2
they originate in the	2
the air is supposed	2
to the interposition of	2
in the preceding pages	2
the report of lieutenant	2
than the cathedral clock	2
her foot on it	2
the requirements of his	2
other part of the	2
belt of rains over	2
stream the fishes rise	2
trade on the north	2
issuing on the north	2
whirling winds the dust	2
northern parts of new	2
round a center of	2
out gently from the	2
published by the smithsonian	2
to three hundred miles	2
what has been said	2
posterior or dry side	2
by the weather bureau	2
the supposed region of	2
in which magnetic action	2
to the huttonian theory	2
of careful observation and	2
same is true in	2
illumed the dewy dell	2
the front of the	2
seed time and harvest	2
and sportive feathers circle	2
the north of them	2
thermometer is up to	2
the earth over which	2
warmth of the ocean	2
the barometer and thermometer	2
after it has passed	2
new mexico and california	2
from any point between	2
belt of rains has	2
urge my perilous course	2
side of the axis	2
with the variations of	2
the difference of seasons	2
to be conducted from	2
if janiveer calends be	2
were not affected by	2
state of things on	2
of the place where	2
in a tabular form	2
breaking of the waves	2
on the face of	2
of cobi and bucharia	2
and the belt of	2
of the earth which	2
the passing of the	2
side of a tree	2
indications of fair weather	2
when the wind veers	2
are the keys of	2
on this day and	2
at the level of	2
forts brooke and moultrie	2
and attracted by the	2
if the first of	2
as the result of	2
for the forces of	2
poles of the magnet	2
no reliance can be	2
is the gathering of	2
the dewy dell last	2
when the southern line	2
in february and march	2
till about the th	2
south of the axis	2
of the pacific ocean	2
the roof of a	2
the quarter from which	2
and the mean of	2
of the great continents	2
storm cloud has passed	2
trade which issues from	2
the primary influence of	2
of the rio grande	2
in still clear weather	2
circle around the moon	2
read to the scientific	2
continues to storm after	2
dare belie the constant	2
on the approach of	2
relation to the weather	2
may seem to be	2
portion of the concentrated	2
same seasons of different	2
when it reached the	2
the action of a	2
the sun can not	2
his tranquil beauty in	2
idea of the different	2
of the summer of	2
that rolls its monthly	2
nor fleecy clouds float	2
chairs and tables crack	2
of july and august	2
did not set clear	2
a house it is	2
the clouds look black	2
the th to the	2
mile above the earth	2
geography of the sea	2
of the clouds of	2
but this is not	2
abbey strikes three minutes	2
series of the caribbean	2
in halos hid her	2
our upper current is	2
negative electricity of the	2
the purpose of the	2
a storm is approaching	2
surface atmosphere of the	2
newport barracks in kentucky	2
is too much for	2
that it would be	2
accepting the invitation of	2
i think i have	2
months in the year	2
the sun is reflected	2
in relation to it	2
bettis said in a	2
what is lightning and	2
months of july and	2
action of the western	2
him the weather man	2
portion of the united	2
overflow of professor dove	2
wind will set in	2
in any other science	2
and the volume of	2
enough south to cover	2
to be the most	2
the length of the	2
from may to september	2
far enough south to	2
one side is a	2
of the magnetic equator	2
temperature was above the	2
belt up to the	2
intense magnetic area of	2
as many times as	2
or three miles of	2
electric state of the	2
of the kew observatory	2
the motion of the	2
like the ocean and	2
if there be one	2
impossible to say that	2
character of the reciprocal	2
east wind and the	2
and in the southern	2
and so are the	2
the place of observation	2
hundred to one hundred	2
they do not blow	2
portion of the country	2
opposite side of the	2
to the formation of	2
rest of the day	2
the mercury in the	2
correspond with the difference	2
shall waft the clouds	2
the indian ocean off	2
the polar belts of	2
of a west india	2
to that of the	2
character of one or	2
the wind during the	2
different periods of the	2
when we come to	2
dense to drop rain	2
methods by which the	2
the collection of facts	2
occur in the storm	2
of the respiratory organs	2
soever the wind may	2
forty or fifty miles	2
when there is not	2
attraction is greatest where	2
i shall be pardoned	2
but if it chance	2
the approach of a	2
ascent of the summer	2
due to its conditions	2
moisture of evaporation which	2
the hills and valleys	2
there is a general	2
be dear all sorts	2
crops have been produced	2
or to the eastward	2
any just conception of	2
the trending of the	2
running toward a storm	2
is a belt of	2
house it is a	2
the winds from the	2
the northern and middle	2
outside of the track	2
the military posts of	2
at other times in	2
as dense as at	2
the tropics toward the	2
before the belt of	2
the rainy and dry	2
which attracts the surface	2
those of the bay	2
is due to the	2
and by reason of	2
talk of the weather	2
northern airs will fan	2
current comes from the	2
belts of showers and	2
moved to the west	2
so shalt thou count	2
the storm investigated by	2
the air from the	2
induced by an increased	2
corn begins to fill	2
the volume of trade	2
to the circular currents	2
and character of storms	2
when they reach the	2
and followed by the	2
out like a lamb	2
pass off to the	2
the fall and winter	2
of june to the	2
which i have seen	2
west of the mountain	2
the new haven tornado	2
of the ohio river	2
distance above the earth	2
same manner as the	2
half of the third	2
of them has been	2
and that the latter	2
the easterly wind will	2
the longitudinal magnetic currents	2
the rain or snow	2
and harvest shall not	2
atmosphere is very clear	2
to the table of	2
producing or governing the	2
the storms and showers	2
having thus taken a	2
of the magnetic needle	2
the area of greatest	2
the depression of temperature	2
of cirrus and cirro	2
of rain makes a	2
varied hues oft wander	2
a gift on the	2
is affected and attracted	2
of the distant worlds	2
north of this line	2
i am not aware	2
which the sun is	2
we may know it	2
each of the four	2
proportion to its length	2
in a single instance	2
ash before the oak	2
at a distance of	2
busy flies disturb the	2
in the atmosphere by	2
about the same height	2
which can not be	2
takes place between the	2
the trade and its	2
cold north polar current	2
we may have a	2
over some portions of	2
the west india hurricanes	2
the maxima and minima	2
east in the morning	2
the north and north	2
wind shall waft the	2
nearer to twelve in	2
storms which are accompanied	2
leeward gulf dash the	2
but it is perfectly	2
limit of the trades	2
of the thermometer for	2
three sides by seas	2
on both sides of	2
as i have been	2
lady of the springe	2
sometimes not more than	2
with a high temperature	2
are supposed to be	2
inches at the level	2
visible sometimes through the	2
knowledge of its origin	2
march is good graffing	2
phenomena of the trade	2
that the lines of	2
wind set in violently	2
at the belt of	2
a great volcanic eruption	2
character of the latter	2
of the arabian sea	2
on the morning of	2
passing south of us	2
a piece under each	2
wander on his brow	2
and over again until	2
over into the other	2
up into the air	2
are indispensable to the	2
you say that it	2
which mark our climate	2
dense as at sea	2
focus of precipitation and	2
are often of this	2
have been produced without	2
the character of one	2
portions of the atmosphere	2
elevations of the barometer	2
wind on its front	2
always in the same	2
thermometer for the year	2
is from some point	2
are usually preceded by	2
to be covered with	2
with blunt horns she	2
phenomena which constitute the	2
you will have a	2
fleecy clouds float lightly	2
as in the west	2
the greater portion of	2
is sometimes the case	2
be observed that in	2
leaps on the noisy	2
line of the belt	2
the gyration of storms	2
not a matter of	2
as the day advanced	2
trades which blow over	2
the light of a	2
as yet but single	2
the moon in halos	2
the interposition of a	2
the smoke from chimneys	2
all signs fail in	2
toward the center of	2
and it is generally	2
which fall annually upon	2
and west of the	2
a thing about it	2
every where over the	2
if the grass grow	2
or lines of equal	2
so the bland aspect	2
along the eastern side	2
when the earth is	2
the distance of five	2
the storm cloud is	2
base of the mountain	2
earth which the equatorial	2
is perfectly consistent with	2
man in his field	2
of the northern transit	2
in the winter months	2
rio grande to the	2
and the character of	2
at the passing of	2
at the meeting of	2
the midst of a	2
mountain ranges and table	2
will not bear a	2
when there are no	2
holds the dusky air	2
the th and th	2
in violently at s	2
full of positive electricity	2
clouds of our climate	2
about the same time	2
and east in the	2
first new moon in	2
takes place in the	2
influence exerted by the	2
on the north of	2
invitation of a friend	2
a clear understanding of	2
on this side of	2
in the following year	2
is believed to have	2
in some places in	2
summer in the penniless	2
the storm has reached	2
whether it be the	2
from that of the	2
than in those of	2
the influence of which	2
portion of south america	2
a belt of rains	2
the force with which	2
that thence successive spring	2
for the diffusion of	2
ocean off the malabar	2
and attracting influence of	2
shooting pains torment her	2
a village near peterborough	2
the tendency to diseases	2
between that and the	2
all our storms originate	2
beauty in the main	2
the observations of dr	2
connected with the formation	2
is not a little	2
but i have never	2
partaking more or less	2
greater magnetic intensity and	2
less of the character	2
have known it blow	2
interposition of a large	2
however this may be	2
and the clouds are	2
so long as the	2
the rainless deserts of	2
not visible at the	2
the area of magnetic	2
manner in which the	2
the variable winds north	2
who dare belie the	2
that it is always	2
was blowing from the	2
lost his yellow vest	2
for their diffusion and	2
the morning of may	2
to reflect the rays	2
signs fail in a	2
distinct rainy and dry	2
distant worlds around us	2
will fall with a	2
variable winds north of	2
to the surface of	2
and the barbary states	2
expansion of the air	2
with the progress of	2
to diseases of the	2
the result of attraction	2
verge of the antarctic	2
the state of new	2
the time of a	2
in the pacific ocean	2
over the entire surface	2
of the wind during	2
portion of our continent	2
the same seasons of	2
as i have already	2
monsoon of the atlantic	2
weight of the air	2
in the indian territory	2
off at the top	2
who very well can	2
arrangements for the diffusion	2
show an increase of	2
broods in his humid	2
and passing over to	2
moon in the wane	2
what i have got	2
in the new moon	2
to give notice of	2
the clouds of our	2
lying north of the	2
it is assumed that	2
mountains and table lands	2
the gathering elemental strife	2
temperature of the boiling	2
atmospheric conditions and phenomena	2
from its eastern edge	2
of the winds and	2
the sun doth rise	2
it over into the	2
from the magnetic equator	2
there have been but	2
following the belt of	2
awful manifestations of power	2
it is impossible to	2
bartlett thus describes it	2
am not aware that	2
of the rainless region	2
i am well aware	2
action of the storm	2
is from a daguerreotype	2
the sun has long	2
the theory assumes that	2
some say she is	2
during the month of	2
seems to be the	2
countries of equal temperature	2
expansion of the heated	2
the air is calm	2
a primary action in	2
the song of the	2
passing of the trades	2
this is too much	2
and will well repay	2
of the summer lines	2
a meteorological kite the	2
increased progress of the	2
the posterior or dry	2
prior to the setting	2
much to do with	2
to the suddenness of	2
aspect of the tranquil	2
southern edge is carried	2
in all the year	2
know that the earth	2
aerial currents which flow	2
pass to the eastward	2
as that of the	2
normal conditions of the	2
redfield is right in	2
almost to the pole	2
of snow and ice	2
the storm is to	2
if the focus of	2
although it is by	2
will give thee tokens	2
of the ocean in	2
red the sun doth	2
volcanic action is not	2
her corns with shooting	2
rosy month of june	2
sinks his tranquil beauty	2
the storm reaches us	2
a large area for	2
there it will stick	2
the upper portion of	2
upon the eastern portion	2
a storm has passed	2
during set fair weather	2
more or less of	2
the line of smooth	2
best bird that ever	2
and at the same	2
half of the sky	2
at about the same	2
is coming steadily on	2
with the rays of	2
i shall endeavor to	2
from panama to california	2
of precipitation in the	2
with the most delicate	2
the observer must be	2
the atlantic and pacific	2
the condensation is over	2
are of volcanic origin	2
is cold and chill	2
see american journal of	2
you will wish yourself	2
the same proportion to	2
near the philippine islands	2
of the heated air	2
to say that they	2
the man who very	2
of the air from	2
since the settlement of	2
of the tropical belt	2
south of the equatorial	2
it was the custom	2
when the air is	2
all the magnetic elements	2
blowing from the n	2
of water like the	2
are those of the	2
is furnished by the	2
the bow or arch	2
by the circular currents	2
owing to the same	2
of intensity and attraction	2
and then we have	2
during the same decade	2
wind is from the	2
johnny sloman could be	2
off the western coast	2
none shall persuade me	2
third of the distance	2
nearly proportional to the	2
the winds of the	2
while the belt of	2
the mountain ranges and	2
must be careful to	2
volcanic action of the	2
of the new haven	2
one for the mouse	2
to the depth of	2
more the character of	2
on thursday at three	2
give me a valentine	2
the work of our	2
in which it is	2
knows what i have	2
in advance of them	2
down to the chambers	2