55 Web address Data of meteorology

55 Web address Data of meteorology

The following is a collection of web addresses to obtain meteorological data. May be useful:)

Example picture of a streamlined layers 850 mb product www.kma.go.kr

The last Clouds animation

http://www.goes.noaa.gov/sohemi/

Satellite International/Aviation Weather Center

http://aviationweather.gov/obs/sat/intl/ir.shtml

Satellite Globe – BOMBS

http://www.bom.gov.au/reguser/by_prod/satellite/globe_pix.shtml

TRMM – Information Flood – CH 24 hours, 2 days and 1 week

http://trmm.gsfc.nasa.gov/publications_dir/potential_flood_hydro.html

Cloud Coverage – TRMM – EIGHT

http://www.lapanrs.com/SMBA/smba.php?agr=1&hal=3&kat=it&per=hr

Japan Satellite

http://www.jma.go.jp/en/gms/

Satellite image of Kochi

http://weather.is.kochi-u.ac.jp/sat/gms.sea/

Archive For The Cloud – Kochi

http://weather.is.kochi-u.ac.jp/archive-e.html

Cyclone Tracks-Unisys

http://weather.unisys.com/hurricane/

Pacific cyclone climatology

http://www.soest.hawaii.edu/MET/Enso/tropical/tropical.html

Hurricane center – Accu weather

http://hurricane.accuweather.com/hurricane/satellite.asp?region=indon&anim=1&type=ir&basin=wpacific

Tropical Cyclone Summaries

http://www.ncdc.noaa.gov/oa/climate/research/tropical-cyclones.html

Pacific cyclone Track

http://www.hurricanezone.net/typhoons/westpacific/satelliteimagery.html

Joint Typhhon waerning center

http://metocph.nmci.navy.mil/cgi-bin/abpwcreate.cgi?Bulletin=abpw

Track of tropical cyclone

http://podaac.jpl.nasa.gov/cgi-bin/hurr/basin.pl

Disaster

http://www.pirba.ristek.go.id/jenis_bencana.php?intid=17&strlang=ind

SOI Pertanggal

http://www.longpaddock.qld.gov.au/SeasonalClimateOutlook/SouthernOscillationIndex/30DaySOIValues/

Monthly SST anomalies

http://www.emc.ncep.noaa.gov/research/cmb/sst_analysis/images/archive/monthly_anomaly/

SST weekly anomaly

http://www.emc.ncep.noaa.gov/research/cmb/sst_analysis/images/archive/weekly_anomaly/

Indian Ocean Dipole (IOD)

http://www.jamstec.go.jp/frsgc/research/d1/iod/

Forecast SST (ENVY)

http://iri.columbia.edu/climate/forecast/sst/

elNino, LaNina, SOI (ENVY)

http://iridl.ldeo.columbia.edu/maproom/.ENSO/

eLNino, LaNina resource page

http://ggweather.com/enso.htm

ENSO Weekly Update

http://ggweather.com/enso.htm

Oceanic Nino Index (ONI) – Year of ElNino-La Nina

http://www.cpc.ncep.noaa.gov/products/analysis_monitoring/ensostuff/ensoyears.shtml

Tahiti-Darwin SOI Graph

http://gcmd.nasa.gov/KeywordSearch/Metadata.do?Portal=GCMD&KeywordPath= [Parameters% 3A + Topic% 3D% 27ATMOSPHERE% 27% 2 c + Term% 3D% 27ATMOSPHERIC + 27% 2 c% PRESSURE + Variable_Level_1% 3D% 27SEA + LEVEL + PRESSURE% 27% 2 c + Detailed_Variable% 3D% 27SLP% 27] OrigMetadataNode = & GCMD EntryId = & NOAA_NWS_CPC_SOI & MetadataView = & Brief MetadataType = 0 & lbnode = mdlb1

Index of marine (SST, DMI, SOI etc.)

http://ioc3.unesco.org/oopc/state_of_the_ocean/all/

ENSO Wrap-up

http://www.bom.gov.au/climate/enso/

eLNino-LaNina years – Intensity

http://ggweather.com/enso/oni.htm

ESPI – NINO

http://precip.gsfc.nasa.gov/rain_pages/el_nino.html

SYNOP-METAR – PASSWORD

http://www.rwic.und.edu/metresources/synop.html

Data SYNOP, METAR, UPPERWIND Weather rankings etc, OGIMET

http://www.rwic.und.edu/metresources/synop.html

PDO, MJO

http://ggweather.com/enso/mjo.htm

Index of the Monsoon, the MJO index etc.

http://www.cpc.ncep.noaa.gov/products/precip/CWlink/MJO/index.primjo.html

MJO, Current condition, weekly report, etc.

http://www.ncdc.noaa.gov/oa/climate/research/tropical-cyclones.html

MJO-Prediction

http://www.cpc.ncep.noaa.gov/products/precip/CWlink/MJO/mjo_chi.shtml

Scheme Of The MJO

http://www.bom.gov.au/bmrc/clfor/cfstaff/matw/maproom/RMM/eof1and2.htm

Archive of a streamlined, isobars

http://www.bom.gov.au/nmoc/MSL/index.shtml

A collection of animated a meteorological phenomenon

http://www.educypedia.be/education/climateanimations.htm

Animation Of Meteorology

http://www.highenergygraphics.com/hienergy.php?catID=4

Weather Education Web

http://www.theweatherprediction.com/

Weather Forecasting

http://www.theweatherprediction.com/habyhints/

Digital learning Pusdiklat BMKG

http://dl.pusdiklat.bmg.go.id/

Upper air Sounding

http://www.weather.uwyo.edu/upperair/sounding.html

elnino, lanina

http://www.pmel.noaa.gov/tao/elnino/la-nina-pacific.html

forecast KI, LI, SI, streamline, etc.

http://www.kma.go.kr/ema/ema03/ra2_eng_index.html

SST

http://www.weather.unisys.com/archive/sst/

Satellite imagery

http://bmkg.go.id/BMKG_Pusat/Meteorologi/Citra_Satelit.bmkg

SST analysis

http://www.weather.unisys.com/archive/sst/sst-121118.gif

k index

http://www.kma.go.kr/cht/ra2d/ra2d_asia1_kindex_ft06_pa4_s012.png

Lifted Index

http://www.kma.go.kr/cht/ra2d/ra2d_asia1_lindex_ft06_pa4_s012.png

Showalter index

http://www.kma.go.kr/cht/ra2d/ra2d_asia1_sindex_ft06_pa4_s012.png

RH 500 mb

http://www.bom.gov.au/charts_data/IDY20105/current/RH/500hPa/IDY20105.RH-500hPa.012.png

Streamline 850 mb

http://www.kma.go.kr/cht/ra2d/ra2d_asia1_wnd850_ft06_pa4_s012.png

Website of meteorology Australia

http://www.bom.gov.au/australia/charts/viewer/index.shtml

Three Forms of matter (solid, liquid, and gas)

Three Forms of matter (solid, liquid, and gas)

Everything you see in after them made of material and all the materials on who takes the form of liquid, solid or gas. The material can be changed from one form to another form, for example when a solid ice cream melts and becomes a liquid.

Three forms of matter

All matter is composed of tiny particles called atoms. When two or more atoms join, the atoms that make up molecules. Atoms and molecules combine in different ways to form three types of matter i.e. solid, liquid and gas. This type of matter is called the third extant material. A form of matter that can be experienced by certain substances called phases of matter. Water is the very type of matter we know. The water usually is in a phase of solid (ice), liquid (water) phase and gas phase (steam).

Solid

Solid is a material that has the form and volume (the space occupied by solid, liquid, or gas). There are two main ways of solid particles can be composed, i.e. in rows neat or orderly in the order of which does not necessarily. The solid particles-partikelnya arranged in regular rows of neat called crystals. Common examples of crystals is mostly metal, diamond, ice, and salt crystals. The solid particles-partikelnya are not arranged regularly called amorphous. Amorphous solids are usually shiny or textured elastic. Common examples of amorphous solids are wax, glass, rubber, and plastics. Because the particles are clustered close together partikelnya blends, solids can not easily suppressed — solids cannot be narrowed further by pushing it down.

On solid, the individual particles are not moving fast enough to beat the force of attraction between the particles. The particles vibrate but bound tightly in place.

Liquid substances

Such as solid, liquid has a definite volume. Unlike a solid, a liquid substance will be shaped like the current container. Described as viscous liquid (fluid). Viscous is a substance with which molecules move freely past each other, so that its shape adapts viscous. Like solids, the particles in the liquid is composed in a meeting. Compressed liquid is also difficult.

On liquid, the molecules arranged a meeting. Even so, the particles have enough energy to overcome some of the nearby molecules tarik-menariknya and eased past each other.

Gas

Gas is a form of matter that is easy to change shape and volume. Such as liquid, gas is described as viscous. The particles in the gas quickly spread filling all available space. As there are great distances between the particles of gas, the gas can easily be compressed to reduce the volume.

In gases, the molecules move very quickly and individuals overcome almost all the styles between the particles. The particles move freely in the entire space occupied room.

The definition of ideal Gas

The definition of ideal Gas

Gas is one of the three States of matter and although this form is an integral part of the study of chemistry, this chapter mainly discusses only the relationship between the volume, temperature and pressure in both the gas and ideal gas is real, and the molecular kinetic theory of gases, and not directly chemistry. The main discussion was mainly about the change of physics, and chemical reactions are not discussion. However, the physical properties of a gas depend on its gaseous molecular structure and chemical properties of gas also depends on its structure. Behavior of the gas exists as a single molecule is a good example of relying on the microscopic structure of macroscopic properties.

a. the nature of gases

The properties of gases can be dirangkumkan as follows.

Gas is transparent.

Gas is distributed evenly in any form its spatial spaces.

Gas in the space will give pressure to the walls.

The Volume of gas is equal to the volume of their vessels. If the gas does not undertakes, gas volume will be an infinite magnitude, and the pressure is going to be infinitely small.

Gases diffuse into all directions no matter the pressure out there or not.

When two or more mixed gases, the gases would be distributed evenly.

Gas can be suppressed with the outside pressure. When the outside pressure is reduced, the gas expands.

When heated, gases expand when cooled down will be mengkerut.

From various properties above, the most important thing is the pressure of the gas. Suppose a liquid filled containers. When a liquid is cooled down and the volume of liquid is reduced, it will not satisfy the container again. However, the gas will always fulfil space no matter regardless of the temperature. That will be changed is the emphasis.

Tools used to measure gas pressure is a manometer. The prototype of the atmospheric pressure gauge, barometer, created by Torricelli.

Pressure is defined as force per unit area, so pressure = force/area.

In SI, the unit of force is the Newton (N), unit area m2, and the unit of pressure is the Pascal (Pa). 1 atm is approximately equal to the pressure of 1013 hPa.

1 atm = 1,01325 x 105 Pa = 1013,25 hPa

However, in units of non-SI units, Torr, roughly 1/760 of 1 atm, often used to measure the change of pressure in chemical reactions (www.chem-is-try.org)

b. Volume and pressure

The fact that the volume of a gas is changed when the pressure change has been observed since the 17th century by the French philosopher and Torricelli/saintis Blase Pascal (1623-1662). Boyle observed that by wearing the pressure with a certain volume of mercury, the volume of gas trapped in a tube closed at delas one end, would be reduced. In this experiment, the volume of gas measured at a pressure greater than 1 atm.

Boyle makes vacuum pumps use engineering tercangih is the time, and he observed that gas at pressures below 1 atm will expand. After he did a lot of experiments, Boyle suggested equations (6.1) to describe the relationship between pressure and volume V P of the gas. This relationship is known as Boyle's law.

PV = k (a constant) (6.1)

Graphical appearance of Boyle's experiments can be done in two ways. When P is plotted as ordinat and V as the absis, obtained a Hyperbola

c. Volume and temperature

After more than a century the discovery of Boyle's scientist got interested in the relationship between the volume and temperature of the gas. Perhaps because of thermal balloon became the topic of conversation in kotakota that time. French chemist Jacques Alexandre César Charles (1746-1823), a navigator's famous balloons at that time, to recognize that, at fixed pressure, volume of gas will increase when the temperature is raised. This relationship is called Charles's law, even though the data is not quantitative. Gay-Lussac was the one who then memplotkan the volume of gas against temperature and get a straight line (Figure 6.2). For this reason Charles's law is often called Gay-Lussac's law. Both Charles's law and law of Gay-Lussac roughly followed by all gas during condensation does not occur.

THE FUNCTION MAP

THE FUNCTION MAP

indicates a position or relative location on the Earth's surface

shows the size of the area and the distance on the Earth's surface

describe the shape of the Earth's surface

presents data for potential areas of

storing and communicating spatial information

help a job

help in making a design

help the analysis of spatial data

THE PROJECTION MAP

based on the Windows will arise

zenital/azimuthal = flat areas (Polar)

cylinder = tubes (Equator)

Cone/conical Cone = (latitude are)

based on the projection field layout

normal/polair

tranversal/azimuthal

oblique/slant

based on the nature of the original is retained

ekuidistan (distance)

konform (shape and direction)

equivalent (area)

based on x-ray source

gnomonic = globe Center

stereografik = polar

orthomorphic = infinity

FACTORS THAT CAN BE READ ON A MAP

FACTORS THAT CAN BE READ ON A MAP

a staple on the horizon

distance

direction

location

parallel meridians = by observing parallel (latitude) and the meridian (line of longitude)

direction and distance

the distance with the distance

height

direction and direction

position = specifies where resection we stand in the field of the unknown on the map. With the help of two points that are identified either on the map or in the field.

intersection = specifies an appearance that does not exist in the map, but there are in the field with the help of two well known point in field as well as on the map.

LOOKING FOR SCALE

compare the points on a map with dots in field

compare it with other existing maps his scale

P2 = (D1/D2) x P1

d1 = the distance on the map is already known

d2 = the distance searched his scale dipeta

p1 = the denominator known map scale

p2 = the map scale denominator is sought

take into account the difference in degrees of latitude

10 = 60 ' = 111km

Ex: difference 5 ' then

the difference then 5 ° 5 ' = (5 ° e/60) x 111

for topographic maps

Ci = (1/2000) x the denominator allusions