Extratropical cyclone PDF

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/Dest (G996747) arctic airmass entrenched E...) /Last 136 0 R /Last 172 0 R }��P�C�FD��F��{?U]mZ��b��6��dF��§� W ��x�U�h��48~|��Ԫ��D�׫��%��r�\L+\}}u�RK'�K7�c!��o(��;�=�V7y��h��]�Ľ�V��l��r>CI��S9_M�g��Q�{E�M܍�<< �@��p�� vd��>h�bj��$R�a��¤9�I� ��t�׈u�h�B5 �bǨ�P�{��y�p��F��(��ݴ��⢈ׂ+ �X 6�߻h}��? ated with fronts:) /Prev 179 0 R

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/Dest (G997529) A signiﬁcant number of tropical cyclones move into the midlatitudes and transform into extratropical cyclones. 0000026603 00000 n >> in the warm air, so surface...) Extratropical cyclones have been found to account for about half of the warm season precipitation over the United States(Heideman and Fritsch, 1988), and the warm conveyor belts associated with these cyclones produce approximately half of the wintertime precipitation in middle and high latitudes (Eckhardt et al., 2004).Thus these storms, also referred to as mid-latitude cyclones, play … 0000002966 00000 n endobj /Next 181 0 R endobj /Prev 176 0 R %PDF-1.4 %�� 0000002900 00000 n /Prev 186 0 R

wind above it.)

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/V 192 0 R 195 0 obj /Title (\200 Front, marked by a shift to warmer SW wind and often some clearing.\ 0000012852 00000 n endobj << �BBP%� "U�AA��jqP�3�JB��@�"5��zq�c1��YD�'n� ��-~9�y�� 5 K$�A��ᗠ5.��8xq��%9K�K*�X��:��p�{��I�g�hZ��Υ��_Z��D��O|�d��O�Z��y��{�g�5�gj��7��|v`�[�f��Z>��>w��U>g|~��b�x��W/xq�ş)Rʃ��BH!GBnQ��￴�%ӟ�?͆rhɴ[/+_��Vĭ��W��W��:��+�V~�j٪��̫&V��/�>�z�ï�f{��k?�9�F�Ƶ�g��Z��x� ��?g��soR�Ծ��e�?��[�3a��a�a��ڴssS��'6�%�ׇ��S!bmDI�%�-bz˺-�-�-w��b[n�ߚ��վ�۷��E�$��zlw%�hg��Ie�%ye4�I�-��)�RS�֍�;�|O��q{�LO~>��J�y��00�{�2F��'�-0�B6�T"X �� d�2��X;� &!�0��L&��0�ĕ�/��c�x)z >> 0000014602 00000 n endobj /Parent 143 0 R /Rotate 90 /Resources 198 0 R 0000012151 00000 n /First 132 0 R y are often less distinct...) /Encoding /WinAnsiEncoding 188 0 obj 0000004487 00000 n >> /Title (\200 Falling temperatures) /Last 159 0 R << >> >> 205 0 obj /R [ 63 9 603 774 ] 199 0 obj 0000088368 00000 n << >> %PDF-1.3 This category has the following 15 subcategories, out of 15 total. /P 26 0 R 0000007989 00000 n /Title (\200 Steady precipitation developing, possibly starting as snow, then ch\ 0000002725 00000 n << 174 0 obj

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An extratropical cyclone (also called a mid-latitude cyclone) is a type of cyclone. 0000011757 00000 n 0000010409 00000 n /Prev 158 0 R 0000009311 00000 n

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>> 0000009190 00000 n 180 0 obj • An extratropical cyclone tends to focus the temperature contrasts into ‘fron-tal zones’ of particularly rapid horizontal temperature change. 0000006298 00000 n /Last 140 0 R /Parent 164 0 R >> /Next 157 0 R /Prev 175 0 R

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subtropical air rises over ...) /R [ 63 9 603 774 ] 0000026545 00000 n 150 0 obj /Parent 178 0 R <<

<< >> 157 0 obj /First 144 0 R /First 135 0 R << /Title (While cold fronts are very distinctive in the Midwest or Eastern US, the\

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endobj /First 137 0 R endobj 0000013317 00000 n /First 171 0 R drop in mountain snow line.) /Next 185 0 R Extratropical Cyclones) endobj >> m fronts near the low cen...) /Parent 164 0 R They have a primary role in determining the local weather and its typical variation, with a strong inﬂuence on precipitation, cloudiness, radiation, and their spatio-tem-poral variability. /Count -2 /Title (\200 because they are trapped against mountains or high ground $E of Ro\

Intense means that near surface sustained2 wind speeds exceed 17 ms¡1 (60 km h¡1, 32 kn). endobj /Dest (G997179) /Dest (G997372) x��MHa��ї��$T&R��+S�e�L b�}w�g��-E"��u�.VD��N�C�:D�u��E^"��;��cT�03�y��|�� U�R�cE4`�λ�ޘvztL��U�F$�s:��k�-iYj��6|�v�P4*wd>,y�4�!7�C�N�-��l��C��T�S�3�q";�-E#+c> �vڴ��=�S԰��79ڸ��@�`Ӌ�m��v�Ul�5��`�P��=��G��j��)�k�P*}�6� ~^/�~�.�~�a��2

>> /Dest (G996782) /First 168 0 R They are low-pressure systems with associated cold fronts, warm fronts, and occluded fronts. 4 0 obj

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/Title (In addition to rapid temperature changes, the following are often associ\ /Dest (G997540) /Next 146 0 R 0000070090 00000 n /Prev 134 0 R << /Title (\200 Characteristic patterns of clouds and precipitation) 0000006800 00000 n endobj

Extra-tropical cyclones are dominant feature of the mid-latitudes, as their passage is associated with strong winds, precipitation, and temperature changes. rom S ahead of front, col...) /Count -2 8rʶ��d�WT'��eL�~.u"A��=9�뗚]��>31�3��X3��-$e�}��u,��gm�g�6�64$ы��EzL*LZ�_�j��_��]�X��y�[�?�Xs ��N��/��]��|m��sϚƫk_Wf��ȸA�2��)�o��z-di��2�|m٣��j|5ԥej�8�ɮe�E��7��[��Q�|�IM%ײ�xf)�|6\ k��`Ҳ��䍐. endobj 0000089877 00000 n

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