Whats My IP Address?

INFORMATION ABOUT IP ADDRESS

Our visitors need to know their IP address for many reasons including gaming, tech support, remote desktop connection, proxy detection, anonymity, or simply to see if their address has changed. Visitors often come here to do an IP Address Lookup to find the location of an IP address. Some folks might've gotten a spam email and want to learn How To Trace An Email. Others might ask themselves How Do I Change My IP. Whatever your reason for visiting, welcome. If you don't find what you're looking for, please Join The What Is My IP Address Forum where you can post your questions and get personal responses.

Internet Protocol Address:

This number is an exclusive number all information technology devices (printers, routers, modems, et al) use which identifies and allows them the ability to communicate with each other on a computer network. There is a standard of communication which is called an Internet Protocol standard. In laymans terms it is the same as your home address. In order for you to receive snail mail at home the sending party must have your correct mailing address (IP address) in your town (network) or you do not receive bills, pizza coupons or your tax refund. The same is true for all equipment on the internet. Without this specific address, information cannot be received. IP addresses may either be assigned permanently for an Email server/Business server or a permanent home resident or temporarily, from a pool of available addresses (first come first serve) from your Internet Service Provider. A permanent number may not be available in all areas and may cost extra so be sure to ask your ISP.

Domain Name System (DNS): This allows the IP address to be translated to words. It is much easier for us to remember a word than a series of numbers. The same is true for email addresses.
For example, it is much easier for you to remember a web address name such as whatismyip.com than it is to remember 192.168.1.1 or in the case of email it is much easier to remember email@somedomain.com than email@192.168.1.1

Dynamic IP Address: One that is not static and could change at any time. This type is issued to you from a pool of addresses allocated by your ISP or DHCP Server. This is for a large number of customers that do not require the same address all the time for a variety of reasons. Your computer will automatically get this number as it logs on to the network and saves you the trouble of having to know details regarding the specific network configurations. This number can be assigned to anyone using a dial-up connection, Wireless and High Speed Internet connections. If you need to run your own email server or web server, it would be best to have a static IP address.
Static IP Address: One that is fixed and never changes. This is in contrast to a dynamic IP address which may change at any time. Most ISP's can offer to assign a single static IP or a block of static IP's for a few extra bucks a month and may require you upgrading to a business account.
IPv4: Currently used by most network devices. However, with more and more computers accessing the internet, IPv4 IPs are running out quickly. Just like in a city, addresses have to be created for new neighborhoods but, if your neighborhood gets too large, you will have to come up with an entire new pool of addresses. IPv4 is limited to 4,294,967,296 IPs.

IPv5: This is an experimental protocol for UNIX based systems. In keeping with standard UNIX (a computer Operating System) release conventions, all odd-numbered versions are considered experimental. It was never intended to be used by the general public.
IPv6: The replacement for the aging IPv4. The estimated number of unique IPs for IPv6 is 340,282,366,920,938,463,463,374,607,431,768,211,456 or 2^128.

The old and current standard of IPs was this: 192.168.100.100 the new way can be written different ways but means the same and are all valid:
* 1080:0000:0000:0000:0000:0034:0000:417A
* 1080:0:0:0:0:34:0:417A
* 1080::34:0:417A

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How do I change my IP address?

"How do I change my IP address?" and "Can I change my IP address?" are probably the most commonly asked questions. Please attempt the following then, if that does not work, visit the Change IP Address forum.
Before trying any other methods to change your IP address, try turning off (or unplugging the power of) your Cable/DSL modem for five minutes. In many cases this will change your IP address. However, if that does not change your IP address, repeat the process for 8 hours (overnight works well) instead of 5 minutes. Hopefully this will result in an IP change.
If the above does not result in your IP address changing, please look through the below for the situation that best matches yours and attempt to change your IP address that way. Unfortunately you are not able to get your IP address to change in all cases, as it is ultimately determined by your ISP's DHCP configuration (when you've got a dynamically assigned IP address, that is.)

Windows

- Computer connected directly to the modem

1= Get to a command prompt. (START, run, cmd).

 

1. Type "ipconfig /release" (without the quotes, on the command line by itself).
2. Type "ipconfig /renew" (without the quotes, on the command line by itself).

3. Windows (second option)

   Windows (second option)

   - Computer connected directly to the modem
4. Get to a command prompt. (START, run, cmd).
5. Type "ipconfig /release" (without the quotes).
6. Shut down computer.
7. Turn off computer.
8. Turn off all ethernet hubs/switches.
9. Turn off cable/DSL modem.
10. Leave off overnight.
11. Turn everything back on.

Network with Router

1. Log into the router's admin console. (Often http://192.168.1.1/)
2. Release the IP address. (Method varies by router manufacturer)
3. Turn off router, ethernet hubs/switches, and the cable/DSL modem.
4. Leave off overnight.
5. Turn everything back on.

If you are using a cable/DSL modem and a router, you may wish to connect your computer directly to the cable/DSL modem. Please note that this could significantly impact your system security. This allows your ISP's DHCP to issue you a new (hopefully changed) IP address based of the (hardware) MAC address of your computer's ethernet card.
If all the above has not worked to change your IP address and you have a router, check and see if there is a "Clone MAC Address" option. Using it should change your IP address; however, you'll only be able to do it once (in most cases).
These will not work in all cases. If all else fails contact your internet service provider (ISP) and ask them if they are able to change your IP address or how long your connection needs to be off for your IP address to change.
If you trying to change your IP address because you are just trying to access web based forums you may wish to attempt to configure your internet browser to use a proxy server.

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What is Google AdWords?

INFORMATION ABOUT G.ADWORDS

So what is Google Adwords and why should I consider using it?

With Google AdWords, you can create and run ads for your business, quickly and simply. Run your ads on Google and our advertising network -- no matter what your budget, you'll only pay when people click your ads. Just visit www.adwords.google.com to get started.
AdWords ads are displayed along with search results when someone searches Google using one of your keywords. Ads appear under 'Sponsored links' in the side column of a search page, and may also appear in additional positions above the free search results. That way, you'll be advertising to an audience that's already interested in your business. You can also choose to display your ads on Display Network sites in the growing Google Network. And, you can choose the exact Display Network placements where you'd like your ad to appear, or you can let contextual targeting match your keywords to content.
You can choose from a variety of ad formats, including text, image, and video ads, and easily track your ad performance using the reports available in your account.

There's no minimum monthly charge with AdWords -- just a nominal activation fee. Learn more about the cost of advertising with Google AdWords. Alternatively, you can watch this short, online course now and get step-by-step instructions on how to create an AdWords account.
To find out more about Google AdWords or to begin creating your ads, visit the AdWords home page.


If you'd like to start advertising and you're looking for an agency to help, you might consider using a Google AdWords Certified Partner. Learn more about AdWords Certified Partners or visit Google Partner Search to locate a list of professionals to suit your requirements. Alternatively, you can watch this short, online course now and get step-by-step instructions on how to create an AdWords account.

You create your ads:

You create ads and choose keywords, which are words or phrases related to your business.

Your ads appear on Google:

When people search on Google using one of your keywords, your ad may appear next to the search results. Now you're advertising to an audience that's already interested in you.

You attract customers:

People can simply click your ad to make a purchase or learn more about you. You don't even need a webpage to get started – Google will help you create one for free. It's that easy!

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Information About Auto Open Arctic Passage

This year's opening marks the fourth time in five years that the Northeast Passage has opened, and commercial shipping companies are taking note. Two German ships recently are the first commercial voyage ever made through the Northeast Passage without the help of icebreakers. The Northeast Passage trims 4,500 miles off the 12,500-mile trip through the Suez Canal, yielding considerable savings in fuel. The voyage was not possible last year, because Russia had not yet worked out a permitting process. With Arctic sea ice expected to continue to decline in the coming decades, shipping traffic through the Northeast Passage will likely become commonplace most summers. The Northeast Passage has remained closed to navigation, except via assist by icebreakers, from 1553 to 2005. The results published in the American Association for the Advancement of Science suggest that prior to 2005, the last previous opening was the period 5,000 - 7,000 years ago, when the Earth's orbital variations brought more sunlight to the Arctic in summer than at present. It is possible we'll know better soon. A new technique that examines organic compounds left behind in Arctic sediments by diatoms that live in sea ice give hope that a detailed record of sea ice extent extending back to the end of the Ice Age 12,000 years ago may be possible (Belt et al., 2007). The researchers are studying sediments along the Northwest Passage in hopes of being able to determine when the Passage was last open.


 The past decade was the warmest decade in the Arctic for the past 2,000 years, according to a study called "Recent Warming Reverses Long-Term Arctic Cooling" published in the journal Science. Four of the five warmest decades in the past 2,000 years occurred between 1950 - 2000, despite the fact that summertime solar radiation in the Arctic has been steadily declining for the past 2,000 years. Previous efforts to reconstruct past climate in the Arctic extended back only 400 years, so the new study--which used lake sediments, glacier ice cores, and tree rings to look at past climate back to the time of Christ, decade by decade-- is a major new milestone in our understanding of the Arctic climate. The researchers found that Arctic temperatures steadily declined between 1 A.D. and 1900 A.D., as would be expected due to a 26,000-year cycle in Earth's orbit that brought less summer sunshine to the North Pole. Earth is now about 620,000 miles (1 million km) farther from the Sun in the Arctic summer than it was 2000 years ago. However, temperatures in the Arctic began to rise around the year 1900, and are now 1.4°C (2.5°F) warmer than they should be, based on the amount of sunlight that is currently falling in the Arctic in summer. "If it hadn't been for the increase in human-produced greenhouse gases, summer temperatures in the Arctic should have cooled gradually over the last century,” According to Bette Otto-Bliesner, a co-author from the National Center for Atmospheric Research.

 Arctic sea ice suffered another summer of significant melting in 2009, with August ice extent the third lowest on record, according to the National Snow and Ice Data Center. August ice extent was 19% below the 1979 - 2000 average, and only 2007 and 2008 saw more melting of Arctic sea ice. We've now had two straight years in the Arctic without a new record minimum in sea ice. However, this does not mean that the Arctic sea ice is recovering. The reduced melting in 2009 compared to 2007 and 2008 primarily resulted from a different atmospheric circulation pattern this summer. This pattern generated winds that transported ice toward the Siberian coast and discouraged export of ice out of the Arctic Ocean. The previous two summers, the prevailing wind pattern acted to transport more ice out of the Arctic through Fram Strait, along the east side of Greenland. At last December's meeting of the American Geophysical Union, the world's largest scientific conference on climate change, J.E. Kay of the National Center for Atmospheric Research showed that Arctic surface pressure in the summer of 2007 was the fourth highest since 1948, and cloud cover at Barrow, Alaska was the sixth lowest. This suggests that once every 10 - 20 years a "perfect storm" of weather conditions highly favorable for ice loss invades the Arctic. The last two times such conditions existed was 1977 and 1987, and it may be another ten or so years before weather conditions align properly to set a new record minimum.




As a result of this summer's melting, the Northeast Passage, a notoriously ice-choked sea route along the northern Russia, is now clear of ice and open for navigation. Satellite analyses by the University of Illinois Polar Research Group and the National Snow and Ice Data Center show that the last remaining ice blockage along the north coast of Russia melted in late August, allowing navigation from Europe to Alaska in ice-free waters. Mariners have been attempting to sail the Northeast Passage since 1553, and it wasn't until the record-breaking Arctic sea-ice melt year of 2005 that the Northeast Passage opened for ice-free navigation for the first time in recorded history. The fabled Northwest Passage through the Arctic waters of Canada has remained closed this summer, however. An atmospheric pressure pattern set up in late July that created winds that pushed old, thick ice into several of the channels of the Northwest Passage. Recent research by Stephen Howell at the University of Waterloo in Canada shows that whether the Northwest Passage clears depends less on how much melt occurs, and more on whether multi-year sea ice is pushed into the channels. Counter-intuitively, as the ice cover thins, ice may flow more easily into the channels, preventing the Northwest Passage from regularly opening in coming decades, if the prevailing winds set up to blow ice into the channels of the Passage. The Northwest Passage opened for the first time in recorded history in 2007, and again in 2008. Mariners have been attempting to find a route through the Northwest Passage since 1497.
 
WASHINGTON, Sept (Reuters) - Climate-warming greenhouse gas emissions pushed Arctic temperatures in the last decade to the highest levels in at least 2,000 years, reversing a natural cooling trend that should have lasted four more millennia.

Carbon dioxide and other gases generated by human activities overwhelmed a 21,000-year cycle linked to gradual changes in Earth's orbit around the Sun, an international team of researchers reported on Thursday in the journal Science.


"I think it really underscores how sensitive the Arctic is to climate change ... and it's really the place where you can see first what's happening to the (climate) system and how the rest of the Earth will or might follow," David Schneider, a co-author and a scientist with the U.S. National Center for Atmospheric Research said in a telephone interview.


The big cool-down started about 7,000 years ago, and Arctic temperatures bottomed out during the so-called "Little Ice Age" that lasted from the 16th to the mid-19th centuries, dove-tailing with the start of the Industrial Revolution.


This cooling trend was caused by a characteristic wobble in Earth's orbit that very gradually pushed the Arctic away from the Sun during the northern summer. Earth is now about 620,000 miles (1 million km) farther from the Sun in the Arctic summer than it was 2000 years ago, said Darrell Kaufmann of Northern Arizona University.


This cooling should have continued through the 20th and 21st centuries and beyond as the 21,000-year cycle played out. This latest research confirms that it hasn't.


"If it hadn't been for the increase in human-produced greenhouse gases, summer temperatures in the Arctic should have cooled gradually over the last century," Bette Otto-Bliesner, a co-author from the National Center for Atmospheric Research, said in a statement.


What happens in the Arctic doesn't stay there, since it is among the world's biggest weather makers, sometimes called Earth's air-conditioner. As Arctic sea ice melts in summer, it exposes the darker-colored ocean water, which absorbs sunlight instead of reflecting it, accelerating the warming effect.


Arctic warming also affects land-based glaciers; if these melt, they would contribute to a global rise in sea levels.


Warming in this area could also thaw frozen ground called permafrost, sending methane, a powerful greenhouse gas, into the atmosphere.


Climate scientists have long known that Earth wobbles in its orbit, which affects how much sunlight reaches the Arctic in the summer. This is the first time a large-scale study has tracked decade-by-decade changes in Arctic summer temperatures this far back in time.

To figure this out, researchers looked at natural archives of temperature -- tree rings, ice cores and lake sediments -- along with computer models, which tallied closely with the natural record.


Average summer temperatures in the Arctic have increased by about 3 degrees F (1.66 degrees C) from what they would have been had the long-term cooling trend remained intact.
  

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