Lecture 1315-441 © 2008 15-441 Lecture 7 DNS Copyright © Seth Goldstein, 2008 Based on slides from previous 441 lectures 1.

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Presentation transcript:

Lecture © Lecture 7 DNS Copyright © Seth Goldstein, 2008 Based on slides from previous 441 lectures 1

© Outline DNS Design DNS Today (Extra credit, remind me at end) Lecture 13

© What is DNS? DNS (Domain Name Service) is primarily used to translate human readable names into machine usable addresses, e.g., IP addresses. DNS goal: –Efficiently locate resources. E.g., Map name  IP address –Scale to many users over a large area –Scale to many updates Lecture 13

How resolve name  IP addr? Lecture © 20084

5 Obvious Solutions (1) Why not centralize DNS? Single point of failure Traffic volume Distant centralized database Single point of update Doesn’t scale! Lecture 13

© Obvious Solutions (2) Why not use /etc/hosts? Original Name to Address Mapping –Flat namespace –/etc/hosts –SRI kept main copy –Downloaded regularly Mid 80’s this became untenable. Why? Count of hosts was increasing: machine per domain  machine per user –Many more downloads –Many more updates /etc/hosts still exists. Lecture 13

© Domain Name System Goals Basically a wide-area distributed database (The biggest in the world!) Scalability Decentralized maintenance Robustness Global scope –Names mean the same thing everywhere Don’t need all of ACID –Atomicity –Strong consistency Do need: distributed update/query & Performance Lecture 13

© Programmer’s View of DNS Conceptually, programmers can view the DNS database as a collection of millions of host entry structures: –in_addr is a struct consisting of 4-byte IP addr Functions for retrieving host entries from DNS: –gethostbyname : query key is a DNS host name. –gethostbyaddr : query key is an IP address. /* DNS host entry structure */ struct hostent { char *h_name; /* official domain name of host */ char **h_aliases; /* null-terminated array of domain names */ int h_addrtype; /* host address type (AF_INET) */ int h_length; /* length of an address, in bytes */ char **h_addr_list; /* null-termed array of in_addr structs */ }; Lecture 13

© DNS Message Format Identification No. of Questions No. of Authority RRs Questions (variable number of answers) Answers (variable number of resource records) Authority (variable number of resource records) Additional Info (variable number of resource records) Flags No. of Answer RRs No. of Additional RRs Name, type fields for a query RRs in response to query Records for authoritative servers Additional “helpful info that may be used 12 bytes Lecture 13

© DNS Header Fields Identification –Used to match up request/response Flags –1-bit to mark query or response –1-bit to mark authoritative or not –1-bit to request recursive resolution –1-bit to indicate support for recursive resolution Lecture 13

© DNS Records RR format: (class, name, value, type, ttl) DB contains tuples called resource records (RRs) Classes = Internet (IN), Chaosnet (CH), etc. Each class defines value associated with type For “IN” class: Type=A –name is hostname –value is IP address Type=NS –name is domain (e.g. foo.com) –value is name of authoritative name server for this domain Type=CNAME name is an alias name for some “canonical” name value is canonical name Type=MX value is hostname of mailserver associated with name Lecture 13

© Properties of DNS Host Entries Different kinds of mappings are possible: 1-1 mapping between domain name and IP addr: provolone.crcl.cs.cmu.edu maps to Multiple domain names maps to the same IP addr: and both map to Single domain name maps to multiple IP addresses: aol.com and map to multiple IP addrs. Some valid domain names don’t map to any IP addr: crcl.cs.cmu.edu doesn’t have a host Lecture 13

© DNS Design: Hierarchy Definitions root edunetorgukcom gwuucbcmubu mit cs ece crcl Each node in hierarchy stores a list of names that end with same suffix Suffix = path up tree E.g., given this tree, where would following be stored: Fred.com Fred.edu Fred.cmu.edu Fred.crcl.cs.cmu.edu Fred.cs.mit.edu Lecture 13

© DNS Design: Zone Definitions Single node Subtree Complete Tree Zone = contiguous section of name space E.g., Complete tree, single node or subtree A zone has an associated set of name servers Must store list of names and tree links root edunetorgukcom gwuucbcmubu mit cs ece crcl Lecture 13

© DNS Design: Cont. Zones are created by convincing owner node to create/delegate a subzone –Records within zone stored in multiple redundant name servers –Primary/master name server updated manually –Secondary/redundant servers updated by zone transfer of name space Zone transfer is a bulk transfer of the “configuration” of a DNS server – uses TCP to ensure reliability Example: –CS.CMU.EDU created by CMU.EDU admins –Who creates CMU.EDU or.EDU? Lecture 13

© DNS: Root Name Servers Responsible for “root” zone 13 root name servers –Currently {a-m}.root-servers.net Local name servers contact root servers when they cannot resolve a name Why 13? Lecture 13

Not really 13! Lecture © /08, from Check out anycast)

So Far Database structure –Hierarchy of labels x.y.z –Organized into zones –Zones have nameservers (notice plural!) Database layout –Records which map names  names, names  ip, etc. Programmer API: gethostbyname, … Lecture ©

© Servers/Resolvers Each host has a resolver –Typically a library that applications can link to –Local name servers hand-configured (or DHCP) (e.g. /etc/resolv.conf) Name servers –Either responsible for some zone or… –Local servers Do lookup of distant host names for local hosts Typically answer queries about local zone Lecture 13

© Typical Resolution Client Local DNS server root & edu DNS server ns1.cmu.edu DNS server NS ns1.cmu.edu NS ns1.cs.cmu.edu A www=IPaddr ns1.cs.cmu.edu DNS server Hmm: Notice root server returned NS ns1.cmu.edu Lecture 13

© Typical Resolution Steps for resolving –Application calls gethostbyname() (RESOLVER) –Resolver contacts local name server (S 1 ) –S 1 queries root server (S 2 ) for ( –S 2 returns NS record for cmu.edu (S 3 ) –What about A record for S 3 ? This is what the additional info section is for (PREFETCHING) –S 1 queries S 3 for –S 3 returns A record for Can return multiple A records  What does this mean? Lecture 13

© Lookup Methods Recursive query: Server goes out and searches for more info Only returns final answer or “not found” Iterative query: Server responds with as much as it knows. “I don’t know this name, but ask this server” Workload impact on choice? Root/distant server does iterative Local server typically does recursive requesting host surf.eurecom.fr gaia.cs.umass.edu root name server local name server dns.eurecom.fr authoritative name server dns.cs.umass.edu intermediate name server dns.umass.edu 7 8 iterated query Lecture 13

How to manage workload? Does root nameserver do recursive lookups? What about other zones? What about imbalance in popularity? –.com versus.dj –google.com versus bleu.crcl.cs.cmu.edu? How do we scale query workload? Lecture ©

© Workload and Caching DNS responses are cached –Quick response for repeated translations –Other queries may reuse some parts of lookup E.g., NS records for domains DNS negative queries are cached –Don’t have to repeat past mistakes –E.g., misspellings, search strings in resolv.conf How do you handle updates? Lecture 13

© Workload and Caching DNS responses are cached –Quick response for repeated translations –Other queries may reuse some parts of lookup E.g., NS records for domains DNS negative queries are cached –Don’t have to repeat past mistakes –E.g., misspellings, search strings in resolv.conf Cached data periodically times out –Lifetime (TTL) of data controlled by owner of data –TTL passed with every record Lecture 13

© Typical Resolution Client Local DNS server root & edu DNS server ns1.cmu.edu DNS server NS ns1.cmu.edu NS ns1.cs.cmu.edu A www=IPaddr ns1.cs.cmu.edu DNS server Lecture 13

© Subsequent Lookup Example Client Local DNS server root & edu DNS server cmu.edu DNS server cs.cmu.edu DNS server ftp.cs.cmu.edu A ftp=IPaddr ftp.cs.cmu.edu Lecture 13

© Reliability DNS servers are replicated –Name service available if ≥ one replica is up –Queries can be load balanced between replicas UDP used for queries –Need reliability  must implement this on top of UDP! –Why not just use TCP? Try alternate servers on timeout –Exponential backoff when retrying same server Same identifier for all queries –Don’t care which server responds Lecture 13

So far Hierarchial name space Lecture ©

© Reverse DNS Task –Given IP address, find its name Method –Maintain separate hierarchy based on IP names –Write as in-addr.arpa Why is the address reversed? Managing –Authority manages IP addresses assigned to it –E.g., CMU manages name space in-addr.arpa edu cmu cs bleu crcl unnamed root arpa in-addr Arpa: backronym  Address and Routing Parameter Area Lecture 13

© arpa Name Server Hierarchy At each level of hierarchy, have group of servers that are authorized to handle that region of hierarchy bleu in-addr.arpa a.root-servers.net m.root-servers.net chia.arin.net (dill, henna, indigo, epazote, figwort, ginseng) cucumber.srv.cs.cmu.edu, t-ns1.net.cmu.edu t-ns2.net.cmu.edu mango.srv.cs.cmu.edu (peach, banana, blueberry) Lecture 13

© Prefetching Name servers can add additional data to response Why would they? Lecture 13

© Prefetching Name servers can add additional data to response Why would they? Typically used for prefetching –CNAME/MX/NS typically point to another host name –Responses include address of host referred to in “additional section” Lecture 13

© Mail Addresses MX records point to mail exchanger for a name –E.g. cmu.edu IN MX 10 CMU-MX4.ANDREW.cmu.edu. cmu.edu IN MX 10 CMU-MX5.ANDREW.cmu.edu. Addition of MX record type proved to be a challenge –How to get mail programs to lookup MX record for mail delivery? –Needed critical mass of such mailers –Could we add a new one now? Lecture 13

© Outline DNS Design DNS Today Lecture 13

© Root Zone Generic Top Level Domains (gTLD) =.com,.net,.org, etc… Country Code Top Level Domain (ccTLD) =.us,.ca,.fi,.uk, etc… Root server ({a-m}.root-servers.net) also used to cover gTLD domains –Load on root servers was growing quickly! –Moving.com,.net,.org off root servers was clearly necessary to reduce load  done Aug 2000 –How significant an effect would this have? On load? On performance? Lecture 13

© gTLDs Unsponsored –.com,.edu,.gov,.mil,.net,.org –.biz  businesses –.info  general info –.name  individuals Sponsored (controlled by a particular association) –.aero  air-transport industry –.cat  catalan related –.coop  business cooperatives –.jobs  job announcements –.museum  museums –.pro  accountants, lawyers, and physicians –.travel  travel industry Starting up –.mobi  mobile phone targeted domains –.post  postal –.tel  telephone related Proposed –.asia,.cym,.geo,.kid,.mail,.sco,.web,.xxx –Whatever you want! Is there anything special about.com? What about adding.goldstein as a gTLD? Lecture 13

© New Registrars Network Solutions (NSI) used to handle all registrations, root servers, etc… –Clearly not the democratic (Internet) way –Large number of registrars that can create new domains  However NSI still handles A root server Lecture 13

© Measurements of DNS No centralized caching per site –Each machine runs own caching local server –Why is this a problem? –How many hosts do we need to share cache?  recent studies suggest hosts “Hit rate for DNS:1 - (#DNS/#connections)  80% –Is this good or bad? –Most Internet traffic was Web with HTTP 1.0 What does a typical page look like?  average of 4-5 imbedded objects  needs 4-5 transfers This alone accounts for 80% hit rate! Lower TTLs for A records does not affect performance DNS performance really relies more on NS-record caching Lecture 13

© Measurements of DNS No centralized caching per site –Each machine runs own caching local server –Why is this a problem? –How many hosts do we need to share cache?  recent studies suggest hosts “Hit rate for DNS:1 - (#DNS/#connections)  80% –Is this good or bad? –Most Internet traffic was Web with HTTP 1.0 What does a typical page look like?  average of 4-5 imbedded objects  needs 4-5 transfers This alone accounts for 80% hit rate! Lower TTLs for A records does not affect performance DNS performance really relies more on NS-record caching Lecture 13

© Tracing Hierarchy (1) Dig Program –Allows querying of DNS system –Use flags to find name server (NS) –Disable recursion so that operates one step at a time –All.edu names handled by set of servers unix> dig NS kittyhawk.cmcl.cs.cmu.edu ;; AUTHORITY SECTION: edu IN NS L3.NSTLD.COM. edu IN NS D3.NSTLD.COM. edu IN NS A3.NSTLD.COM. edu IN NS E3.NSTLD.COM. edu IN NS C3.NSTLD.COM. edu IN NS F3.NSTLD.COM. edu IN NS G3.NSTLD.COM. edu IN NS B3.NSTLD.COM. edu IN NS M3.NSTLD.COM. Zone TTL Class Type Value Lecture 13

© Tracing Hierarchy (2) 3 servers handle CMU names unix> dig NS kittyhawk.cmcl.cs.cmu.edu ;; AUTHORITY SECTION: cmu.edu IN NS CUCUMBER.SRV.cs.cmu.edu. cmu.edu IN NS T-NS1.NET.cmu.edu. cmu.edu IN NS T-NS2.NET.cmu.edu. Lecture 13

© Tracing Hierarchy (3 & 4) 4 servers handle CMU CS names Quasar is master NS for this zone unix> dig NS kittyhawk.cmcl.cs.cmu.edu ;; AUTHORITY SECTION: cs.cmu.edu IN NS MANGO.SRV.cs.cmu.edu. cs.cmu.edu IN NS PEACH.SRV.cs.cmu.edu. cs.cmu.edu IN NS BANANA.SRV.cs.cmu.edu. cs.cmu.edu IN NS BLUEBERRY.SRV.cs.cmu.edu. unix>dig NS kittyhawk.cmcl.cs.cmu.edu ;; AUTHORITY SECTION: cs.cmu.edu. 300 IN SOA QUASAR.FAC.cs.cmu.edu. Lecture 13

© DNS (Summary) Motivations  large distributed database –Scalability –Independent update –Robustness Hierarchical database structure –Zones –How lookups are done Caching/prefetching and TTLs Reverse name lookup What are the steps to creating your own domain? Lecture 13