Horrible Result of Global Warming:North Pole could be ice-free this summer, scientists say

The North Pole may be briefly ice-free by September as global warming melts away Arctic sea ice, according to scientists from the National Snow and Ice Data Center in Boulder, Colorado.

Scientists say it’s a 50-50 bet that the thin Arctic sea ice will completely melt away at the geographic North Pole.

“We kind of have an informal betting pool going around in our center and that betting pool is ‘does the North Pole melt out this summer?’ and it may well,” said the center’s senior research scientist, Mark Serreze.

It’s a 50-50 bet that the thin Arctic sea ice, which was frozen in autumn, will completely melt away at the geographic North Pole, Serreze said.

The ice retreated to a record level in September when the Northwest Passage, the sea route through the Arctic Ocean, opened briefly for the first time in recorded history.

“What we’ve seen through the past few decades is the Arctic sea ice cover is becoming thinner and thinner as the system warms up,” Serreze said.
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Posted in Environment, Global Warming, News, water | 1 Comment

Arctic Ice Meltdown Continues With Significantly Reduced Winter Ice Cover

As far as temperatures drop in the Arctic winter – on average to -34°C (-29°F) – a new study shows that in the last two years sea ice is shrinking on the surface of Arctic waters to record low levels. Using satellite data, scientists have observed unusually warm wintertime temperatures in the region and a resulting decline in the length of the Arctic seasonal ice.

Image above:: Summer ice is not the only Arctic ice that has retreated in recent years. In 2005 and 2006, the winter ice maximum was about 6% smaller than the average amount over the past 26 years. This retreat is larger than the long-term 1.5 to 2% decrease in winter ice per decade. This visualization shows the winter sea ice cover during its annual maximum extent from 1979 to 2006, with the edge of the yellow area representing the farthest south reached by the winter ice cover since 1979. Click on image to view animation. Credit: NASA

The maximum amount of sea ice in the Arctic winter has fallen by six percent over each of the last two winters, as compared to a loss of merely 1.5 percent per decade on average annually since the earliest satellite monitoring in 1979. This is happening as summer sea ice continues its retreat at an average of ten percent per decade.

Image left: In this image, the whole of the sea surface is made of forming sea ice. Credit: NASA

“This amount of Arctic sea ice reduction the past two consecutive winters has not taken place before during the 27 years satellite data has been available,” said Joey Comiso, a research scientist at NASA’s Goddard Space Flight Center, Greenbelt, Md. “In the past, sea ice reduction in winter was significantly lower per decade compared to summer sea ice retreat. What’s remarkable is that we’ve witnessed sea ice reduction at six percent per year over just the last two winters, most likely a result of warming due to greenhouse gases.”

Comiso used satellite data from 1978 to 2006 to carry out the study, to be published in Geophysical Research Letters this month.

Computer simulations of the climate warming effect of greenhouse gases had predicted that winter sea ice would decline faster than summer sea ice Satellite data has shown otherwise until two years ago, when record low winter ice cover and warmer temperatures have prevailed.

Sea ice cover in the Norther Hemisphere spans nearly 6.2 million square miles in the winter. Satellite sensors are the only means to observe such a large region effectively. Comiso confirmed the accuracy of satellite sea ice data by comparing it with high-resolution satellite information and data gathered from sensitive instruments aboard aircraft. Surface temperature data from satellite sensors are checked against measurements from meteorological stations in the region.

Adding to the plight of winter sea ice, previous research has shown a trend in which the melt period lasts about two weeks longer per year annually due to summer sea ice decline. This means that the onset of freeze-up is happening later in the fall season. As a result, the ice cover in winter never gets as extensive as it would have been if the freeze-up had begun earlier. More than that, the ice reflects the sun’s radiation much more efficiently than the ocean’s surface. As a result, as the ice cover declines, the ocean’s surface warms, causing in turn, further decline of the ice.
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Topology and Layers in GIS

TOPOLOGY & LAYERS (THEMES)

Topology refers to the spatial relationships between geographic features. It describes the relationships between connecting or
adjacent coverage features. Topological relationships are built from simple elements into complex elements: points
(simplest elements), arcs (sets of connected points), areas (sets of connected arcs), and routes (sets of sections, which are
arcs or portions of arcs).

Topology is useful in GIS because many spatial modeling operations don’t require coordinates, only topological information.
For example, to find an optimal path between two points requires a list of the arcs that connect to each other and the cost to
traverse each arc in each direction. Coordinates are only needed for drawing the path after it is calculated.

Components of Topology:

Topology has three basic components:

I. Connectivity (Arc – Node Topology):

o Points along an arc that define its shape are called Vertices.

o Endpoints of the arc are called Nodes.

o Arcs join only at the Nodes.

II. Area Definition / Containment (Polygon – Arc Topology):

o An enclosed polygon has a measurable area.

o Lists of arcs define boundaries and closed areas are maintained.

o Polygons are represented as a series of (x , y) coordinates that connect to define an area.

III. Contiguity:

o Every arc has a direction

o A GIS maintains a list of Polygons on the left and right side of each arc.

o The computer then uses this information to determine which features are next to one another.

Explanation of Topology:

TOPOLOGY & LAYERS (THEMES)

Topology refers to the spatial relationships between geographic features. It describes the relationships between connecting or
adjacent coverage features. Topological relationships are built from simple elements into complex elements: points
(simplest elements), arcs (sets of connected points), areas (sets of connected arcs), and routes (sets of sections, which are
arcs or portions of arcs).

Topology is useful in GIS because many spatial modeling operations don’t require coordinates, only topological information.
For example, to find an optimal path between two points requires a list of the arcs that connect to each other and the cost to
traverse each arc in each direction. Coordinates are only needed for drawing the path after it is calculated.

Components of Topology:

Topology has three basic components:

I. Connectivity (Arc – Node Topology):

o Points along an arc that define its shape are called Vertices.

o Endpoints of the arc are called Nodes.

o Arcs join only at the Nodes.

II. Area Definition / Containment (Polygon – Arc Topology):

o An enclosed polygon has a measurable area.

o Lists of arcs define boundaries and closed areas are maintained.

o Polygons are represented as a series of (x , y) coordinates that connect to define an area.

III. Contiguity:

o Every arc has a direction

o A GIS maintains a list of Polygons on the left and right side of each arc.

o The computer then uses this information to determine which features are next to one another.

Explanation of Topology:

yers (Themes):

Maps produced traditionally or by automation involved the separation of data into layers, that each contained different types of
features: rivers, roads, etc. These are then combined to form a map where layers have usually been printed in different colors.
To present all the data collected for a given area might require the production of several maps, as they could not all be printed  together. Equally in GIS, data for an area are divided into layers or themes, divided by type but here for the dual purposes of display and analysis.
Themes

The database can be divided into as many layers as is necessary, where each layer contains one characteristic such as soils,  land use, drainage, etc. The layers ‘overlay’ each other perfectly as a result of Georeferencing and enabling analysis between layers.
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Posted in GIS, Remote Sensing 101 | 3 Comments

GPS on a growth path

Global Positioning System (GPS) provides unequaled accuracy and flexibility of positioning for navigation, surveying and geographic information system (GIS) data capture. Its growing use in automotive and consumer applications is propelling the market for mobile location technologies. Although standalone products are quite popular, the most common applications are built around Portable Navigation Devices (PNDs), mobile phones, or car navigation systems. Moreover, the technology is fast gaining acceptance worldwide, as it is penetrating into previously untapped areas. 

GPS companies, both local and international, are competing to grab a piece of this market, especially in logistics for tracking cargo and trucks across India. Lately, the GPS market has started picking up in the country and competition between GPS device providers such as Garmin and inbuilt GPS provider in phone like Nokia has begun. Along with this, we already have maps and static navigation systems available for free or at cheap rates.

Globally, the GPS market is expected to exceed $30 billion in this financial year, as the market is being flooded by a number of affordable GPS components and receivers. As far as the Indian market is concerned, a relatively large number of players have entered the navigation market, which in turn depicts that the potential for development in the market is significant and that the industry will surge in years to come.
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Posted in GPS, News | 1 Comment